The representation of sea salt aerosols and their role in polar climate within CMIP6

International audience Natural aerosols and their interactions with clouds remain an important uncertainty within climate models, especially at the poles. Here, we study the behavior of sea salt aerosols (SSaer) in the Arctic and Antarctic within 12 climate models from CMIP6. We investigate the driv...

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Published in:Journal of Geophysical Research: Atmospheres
Main Authors: Lapere, Rémy, Thomas, Jennie, L, Marelle, Louis, Ekman, Annica, M. L., Frey, Markus, M, Lund, Marianne, Tronstad, Makkonen, Risto, Ranjithkumar, Ananth, Salter, Matthew, E, Samset, Bjørn, Hallvard, Schulz, Michael, Sogacheva, Larisa, Yang, Xin, Zieger, Paul
Other Authors: Institut des Géosciences de l’Environnement (IGE), Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Observatoire des Sciences de l'Univers de Grenoble (Fédération OSUG)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP), Université Grenoble Alpes (UGA), TROPO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Department of Meteorology Stockholm (MISU), Stockholm University, Bolin Centre for Climate Research, British Antarctic Survey (BAS), Natural Environment Research Council (NERC), Center for International Climate and Environmental Research Oslo (CICERO), University of Oslo (UiO), Faculty of Informatics and Mathematics (FMI), Fakultät für Informatik und Mathematik, Norwegian Meteorological Institute Oslo (MET), Finnish Meteorological Institute (FMI), Department of Environmental Science Lancaster, Lancaster University
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2023
Subjects:
Online Access:https://insu.hal.science/insu-04020054
https://insu.hal.science/insu-04020054v2/document
https://insu.hal.science/insu-04020054v2/file/JGR%20Atmospheres%20-%202023%20-%20Lapere%20-%20Sea%20Salt%20Aerosols.pdf
https://doi.org/10.1029/2022jd038235
id ftuniparissaclay:oai:HAL:insu-04020054v2
record_format openpolar
institution Open Polar
collection Archives ouvertes de Paris-Saclay
op_collection_id ftuniparissaclay
language English
topic [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
spellingShingle [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
Lapere, Rémy
Thomas, Jennie, L
Marelle, Louis
Ekman, Annica, M. L.
Frey, Markus, M
Lund, Marianne, Tronstad
Makkonen, Risto
Ranjithkumar, Ananth
Salter, Matthew, E
Samset, Bjørn, Hallvard
Schulz, Michael
Sogacheva, Larisa
Yang, Xin
Zieger, Paul
The representation of sea salt aerosols and their role in polar climate within CMIP6
topic_facet [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
description International audience Natural aerosols and their interactions with clouds remain an important uncertainty within climate models, especially at the poles. Here, we study the behavior of sea salt aerosols (SSaer) in the Arctic and Antarctic within 12 climate models from CMIP6. We investigate the driving factors that control SSaer abundances and show large differences based on the choice of the source function, and the representation of aerosol processes in the atmosphere. Close to the poles, the CMIP6 models do not match observed seasonal cycles of surface concentrations, likely due to the absence of wintertime SSaer sources such as blowing snow. Further away from the poles, simulated concentrations have the correct seasonality, but have a positive mean bias of up to one order of magnitude. SSaer optical depth is derived from the MODIS data and compared to modeled values, revealing good agreement, except for winter months. Better agreement for AOD than surface concentration may indicate a need for improving the vertical distribution, the size distribution and/or hygroscopicity of modeled polar SSaer. Source functions used in CMIP6 emit very different numbers of small SSaer, potentially exacerbating cloud-aerosol interaction uncertainties in these remote regions. For future climate scenarios SSP126 and SSP585, we show that SSaer concentrations increase at both poles at the end of the 21st century, with more than two times mid-20th century values in the Arctic. The pre-industrial climate CMIP6 experiments suggest there is a large uncertainty in the polar radiative budget due to SSaer.
author2 Institut des Géosciences de l’Environnement (IGE)
Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Observatoire des Sciences de l'Univers de Grenoble (Fédération OSUG)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP)
Université Grenoble Alpes (UGA)
TROPO - LATMOS
Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)
Department of Meteorology Stockholm (MISU)
Stockholm University
Bolin Centre for Climate Research
British Antarctic Survey (BAS)
Natural Environment Research Council (NERC)
Center for International Climate and Environmental Research Oslo (CICERO)
University of Oslo (UiO)
Faculty of Informatics and Mathematics (FMI)
Fakultät für Informatik und Mathematik
Norwegian Meteorological Institute Oslo (MET)
Finnish Meteorological Institute (FMI)
Department of Environmental Science Lancaster
Lancaster University
format Article in Journal/Newspaper
author Lapere, Rémy
Thomas, Jennie, L
Marelle, Louis
Ekman, Annica, M. L.
Frey, Markus, M
Lund, Marianne, Tronstad
Makkonen, Risto
Ranjithkumar, Ananth
Salter, Matthew, E
Samset, Bjørn, Hallvard
Schulz, Michael
Sogacheva, Larisa
Yang, Xin
Zieger, Paul
author_facet Lapere, Rémy
Thomas, Jennie, L
Marelle, Louis
Ekman, Annica, M. L.
Frey, Markus, M
Lund, Marianne, Tronstad
Makkonen, Risto
Ranjithkumar, Ananth
Salter, Matthew, E
Samset, Bjørn, Hallvard
Schulz, Michael
Sogacheva, Larisa
Yang, Xin
Zieger, Paul
author_sort Lapere, Rémy
title The representation of sea salt aerosols and their role in polar climate within CMIP6
title_short The representation of sea salt aerosols and their role in polar climate within CMIP6
title_full The representation of sea salt aerosols and their role in polar climate within CMIP6
title_fullStr The representation of sea salt aerosols and their role in polar climate within CMIP6
title_full_unstemmed The representation of sea salt aerosols and their role in polar climate within CMIP6
title_sort representation of sea salt aerosols and their role in polar climate within cmip6
publisher HAL CCSD
publishDate 2023
url https://insu.hal.science/insu-04020054
https://insu.hal.science/insu-04020054v2/document
https://insu.hal.science/insu-04020054v2/file/JGR%20Atmospheres%20-%202023%20-%20Lapere%20-%20Sea%20Salt%20Aerosols.pdf
https://doi.org/10.1029/2022jd038235
geographic Arctic
Antarctic
geographic_facet Arctic
Antarctic
genre Antarc*
genre_facet Antarc*
op_source ISSN: 2169-897X
EISSN: 2169-8996
Journal of Geophysical Research: Atmospheres
https://insu.hal.science/insu-04020054
Journal of Geophysical Research: Atmospheres, 2023, 128 (6), pp.e2022JD038235. ⟨10.1029/2022jd038235⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2022jd038235
doi:10.1029/2022jd038235
op_rights http://creativecommons.org/licenses/by/
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op_doi https://doi.org/10.1029/2022jd038235
container_title Journal of Geophysical Research: Atmospheres
container_volume 128
container_issue 6
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spelling ftuniparissaclay:oai:HAL:insu-04020054v2 2024-10-29T17:40:31+00:00 The representation of sea salt aerosols and their role in polar climate within CMIP6 Lapere, Rémy Thomas, Jennie, L Marelle, Louis Ekman, Annica, M. L. Frey, Markus, M Lund, Marianne, Tronstad Makkonen, Risto Ranjithkumar, Ananth Salter, Matthew, E Samset, Bjørn, Hallvard Schulz, Michael Sogacheva, Larisa Yang, Xin Zieger, Paul Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Observatoire des Sciences de l'Univers de Grenoble (Fédération OSUG)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP) Université Grenoble Alpes (UGA) TROPO - LATMOS Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) Department of Meteorology Stockholm (MISU) Stockholm University Bolin Centre for Climate Research British Antarctic Survey (BAS) Natural Environment Research Council (NERC) Center for International Climate and Environmental Research Oslo (CICERO) University of Oslo (UiO) Faculty of Informatics and Mathematics (FMI) Fakultät für Informatik und Mathematik Norwegian Meteorological Institute Oslo (MET) Finnish Meteorological Institute (FMI) Department of Environmental Science Lancaster Lancaster University 2023 https://insu.hal.science/insu-04020054 https://insu.hal.science/insu-04020054v2/document https://insu.hal.science/insu-04020054v2/file/JGR%20Atmospheres%20-%202023%20-%20Lapere%20-%20Sea%20Salt%20Aerosols.pdf https://doi.org/10.1029/2022jd038235 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2022jd038235 doi:10.1029/2022jd038235 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 2169-897X EISSN: 2169-8996 Journal of Geophysical Research: Atmospheres https://insu.hal.science/insu-04020054 Journal of Geophysical Research: Atmospheres, 2023, 128 (6), pp.e2022JD038235. ⟨10.1029/2022jd038235⟩ [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/article Journal articles 2023 ftuniparissaclay https://doi.org/10.1029/2022jd038235 2024-10-03T23:59:11Z International audience Natural aerosols and their interactions with clouds remain an important uncertainty within climate models, especially at the poles. Here, we study the behavior of sea salt aerosols (SSaer) in the Arctic and Antarctic within 12 climate models from CMIP6. We investigate the driving factors that control SSaer abundances and show large differences based on the choice of the source function, and the representation of aerosol processes in the atmosphere. Close to the poles, the CMIP6 models do not match observed seasonal cycles of surface concentrations, likely due to the absence of wintertime SSaer sources such as blowing snow. Further away from the poles, simulated concentrations have the correct seasonality, but have a positive mean bias of up to one order of magnitude. SSaer optical depth is derived from the MODIS data and compared to modeled values, revealing good agreement, except for winter months. Better agreement for AOD than surface concentration may indicate a need for improving the vertical distribution, the size distribution and/or hygroscopicity of modeled polar SSaer. Source functions used in CMIP6 emit very different numbers of small SSaer, potentially exacerbating cloud-aerosol interaction uncertainties in these remote regions. For future climate scenarios SSP126 and SSP585, we show that SSaer concentrations increase at both poles at the end of the 21st century, with more than two times mid-20th century values in the Arctic. The pre-industrial climate CMIP6 experiments suggest there is a large uncertainty in the polar radiative budget due to SSaer. Article in Journal/Newspaper Antarc* Archives ouvertes de Paris-Saclay Arctic Antarctic Journal of Geophysical Research: Atmospheres 128 6