Evaluation of ocean dimethylsulfide concentration and emission in CMIP6 models

International audience Abstract. Characteristics and trends of surface ocean dimethylsulfide (DMS) concentrations and fluxes into the atmosphere of four Earth system models (ESMs: CNRM-ESM2-1, MIROC-ES2L, NorESM2-LM, and UKESM1-0-LL) are analysed over the recent past (1980–2009) and into the future,...

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Published in:Biogeosciences
Main Authors: Bock, Josué, Michou, Martine, Nabat, Pierre, Abe, Manabu, Mulcahy, Jane, Olivié, Dirk, Schwinger, Jörg, Suntharalingam, Parvadha, Tjiputra, Jerry, van Hulten, Marco, Watanabe, Michio, Yool, Andrew, Séférian, Roland
Other Authors: Groupe de Météorologie de Grande Échelle et Climat (GMGEC), Centre national de recherches météorologiques (CNRM), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2021
Subjects:
Online Access:https://hal.science/hal-03975296
https://hal.science/hal-03975296/document
https://hal.science/hal-03975296/file/bg-18-3823-2021.pdf
https://doi.org/10.5194/bg-18-3823-2021
id ftccsdartic:oai:HAL:hal-03975296v1
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institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
Bock, Josué
Michou, Martine
Nabat, Pierre
Abe, Manabu
Mulcahy, Jane
Olivié, Dirk
Schwinger, Jörg
Suntharalingam, Parvadha
Tjiputra, Jerry
van Hulten, Marco
Watanabe, Michio
Yool, Andrew
Séférian, Roland
Evaluation of ocean dimethylsulfide concentration and emission in CMIP6 models
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
description International audience Abstract. Characteristics and trends of surface ocean dimethylsulfide (DMS) concentrations and fluxes into the atmosphere of four Earth system models (ESMs: CNRM-ESM2-1, MIROC-ES2L, NorESM2-LM, and UKESM1-0-LL) are analysed over the recent past (1980–2009) and into the future, using Coupled Model Intercomparison Project 6 (CMIP6) simulations. The DMS concentrations in historical simulations systematically underestimate the most widely used observed climatology but compare more favourably against two recent observation-based datasets. The models better reproduce observations in mid to high latitudes, as well as in polar and westerlies marine biomes. The resulting multi-model estimate of contemporary global ocean DMS emissions is 16–24 Tg S yr−1, which is narrower than the observational-derived range of 16 to 28 Tg S yr−1. The four models disagree on the sign of the trend of the global DMS flux from 1980 onwards, with two models showing an increase and two models a decrease. At the global scale, these trends are dominated by changes in surface DMS concentrations in all models, irrespective of the air–sea flux parameterisation used. In turn, three models consistently show that changes in DMS concentrations are correlated with changes in marine productivity; however, marine productivity is poorly constrained in the current generation of ESMs, thus limiting the predictive ability of this relationship. In contrast, a consensus is found among all models over polar latitudes where an increasing trend is predominantly driven by the retreating sea-ice extent. However, the magnitude of this trend between models differs by a factor of 3, from 2.9 to 9.2 Gg S decade−1 over the period 1980–2014, which is at the low end of a recent satellite-derived analysis. Similar increasing trends are found in climate projections over the 21st century.
author2 Groupe de Météorologie de Grande Échelle et Climat (GMGEC)
Centre national de recherches météorologiques (CNRM)
Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Bock, Josué
Michou, Martine
Nabat, Pierre
Abe, Manabu
Mulcahy, Jane
Olivié, Dirk
Schwinger, Jörg
Suntharalingam, Parvadha
Tjiputra, Jerry
van Hulten, Marco
Watanabe, Michio
Yool, Andrew
Séférian, Roland
author_facet Bock, Josué
Michou, Martine
Nabat, Pierre
Abe, Manabu
Mulcahy, Jane
Olivié, Dirk
Schwinger, Jörg
Suntharalingam, Parvadha
Tjiputra, Jerry
van Hulten, Marco
Watanabe, Michio
Yool, Andrew
Séférian, Roland
author_sort Bock, Josué
title Evaluation of ocean dimethylsulfide concentration and emission in CMIP6 models
title_short Evaluation of ocean dimethylsulfide concentration and emission in CMIP6 models
title_full Evaluation of ocean dimethylsulfide concentration and emission in CMIP6 models
title_fullStr Evaluation of ocean dimethylsulfide concentration and emission in CMIP6 models
title_full_unstemmed Evaluation of ocean dimethylsulfide concentration and emission in CMIP6 models
title_sort evaluation of ocean dimethylsulfide concentration and emission in cmip6 models
publisher HAL CCSD
publishDate 2021
url https://hal.science/hal-03975296
https://hal.science/hal-03975296/document
https://hal.science/hal-03975296/file/bg-18-3823-2021.pdf
https://doi.org/10.5194/bg-18-3823-2021
genre Sea ice
genre_facet Sea ice
op_source ISSN: 1726-4170
EISSN: 1726-4189
Biogeosciences
https://hal.science/hal-03975296
Biogeosciences, 2021, 18 (12), pp.3823-3860. ⟨10.5194/bg-18-3823-2021⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/bg-18-3823-2021
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doi:10.5194/bg-18-3823-2021
op_rights http://creativecommons.org/licenses/by/
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op_doi https://doi.org/10.5194/bg-18-3823-2021
container_title Biogeosciences
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spelling ftccsdartic:oai:HAL:hal-03975296v1 2023-12-24T10:24:48+01:00 Evaluation of ocean dimethylsulfide concentration and emission in CMIP6 models Bock, Josué Michou, Martine Nabat, Pierre Abe, Manabu Mulcahy, Jane Olivié, Dirk Schwinger, Jörg Suntharalingam, Parvadha Tjiputra, Jerry van Hulten, Marco Watanabe, Michio Yool, Andrew Séférian, Roland Groupe de Météorologie de Grande Échelle et Climat (GMGEC) Centre national de recherches météorologiques (CNRM) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) 2021 https://hal.science/hal-03975296 https://hal.science/hal-03975296/document https://hal.science/hal-03975296/file/bg-18-3823-2021.pdf https://doi.org/10.5194/bg-18-3823-2021 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/bg-18-3823-2021 hal-03975296 https://hal.science/hal-03975296 https://hal.science/hal-03975296/document https://hal.science/hal-03975296/file/bg-18-3823-2021.pdf doi:10.5194/bg-18-3823-2021 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 1726-4170 EISSN: 1726-4189 Biogeosciences https://hal.science/hal-03975296 Biogeosciences, 2021, 18 (12), pp.3823-3860. ⟨10.5194/bg-18-3823-2021⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere info:eu-repo/semantics/article Journal articles 2021 ftccsdartic https://doi.org/10.5194/bg-18-3823-2021 2023-11-25T23:51:49Z International audience Abstract. Characteristics and trends of surface ocean dimethylsulfide (DMS) concentrations and fluxes into the atmosphere of four Earth system models (ESMs: CNRM-ESM2-1, MIROC-ES2L, NorESM2-LM, and UKESM1-0-LL) are analysed over the recent past (1980–2009) and into the future, using Coupled Model Intercomparison Project 6 (CMIP6) simulations. The DMS concentrations in historical simulations systematically underestimate the most widely used observed climatology but compare more favourably against two recent observation-based datasets. The models better reproduce observations in mid to high latitudes, as well as in polar and westerlies marine biomes. The resulting multi-model estimate of contemporary global ocean DMS emissions is 16–24 Tg S yr−1, which is narrower than the observational-derived range of 16 to 28 Tg S yr−1. The four models disagree on the sign of the trend of the global DMS flux from 1980 onwards, with two models showing an increase and two models a decrease. At the global scale, these trends are dominated by changes in surface DMS concentrations in all models, irrespective of the air–sea flux parameterisation used. In turn, three models consistently show that changes in DMS concentrations are correlated with changes in marine productivity; however, marine productivity is poorly constrained in the current generation of ESMs, thus limiting the predictive ability of this relationship. In contrast, a consensus is found among all models over polar latitudes where an increasing trend is predominantly driven by the retreating sea-ice extent. However, the magnitude of this trend between models differs by a factor of 3, from 2.9 to 9.2 Gg S decade−1 over the period 1980–2014, which is at the low end of a recent satellite-derived analysis. Similar increasing trends are found in climate projections over the 21st century. Article in Journal/Newspaper Sea ice Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Biogeosciences 18 12 3823 3860