Using ship-borne observations of methane isotopic ratio in the Arctic Ocean to understand methane sources in the Arctic

International audience Characterizing methane sources in the Arctic remains challenging due to the remoteness, heterogeneity and variety of such emissions. In situ campaigns provide valuable datasets to reduce these uncertainties. Here we analyse data from the summer 2014 SWERUS-C3 campaign in the e...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Berchet, Antoine, Pison, Isabelle, Crill, Patrick, Thornton, Brett, Bousquet, Philippe, Thonat, Thibaud, Hocking, Thomas, Thanwerdas, Joël, Paris, Jean-Daniel, Saunois, Marielle
Other Authors: Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Modélisation INVerse pour les mesures atmosphériques et SATellitaires (SATINV), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-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)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), ICOS-RAMCES (ICOS-RAMCES), Bolin Centre for Climate Research, Stockholm University, This research has been supported by the Franco-Swedish project IZOMET-FS (grant no. VR 2014-6584).
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2020
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-02532741
https://hal.archives-ouvertes.fr/hal-02532741/document
https://hal.archives-ouvertes.fr/hal-02532741/file/acp-20-3987-2020.pdf
https://doi.org/10.5194/acp-20-3987-2020
id ftccsdartic:oai:HAL:hal-02532741v1
record_format openpolar
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
[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
Berchet, Antoine
Pison, Isabelle
Crill, Patrick
Thornton, Brett
Bousquet, Philippe
Thonat, Thibaud
Hocking, Thomas
Thanwerdas, Joël
Paris, Jean-Daniel
Saunois, Marielle
Using ship-borne observations of methane isotopic ratio in the Arctic Ocean to understand methane sources in the Arctic
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 Characterizing methane sources in the Arctic remains challenging due to the remoteness, heterogeneity and variety of such emissions. In situ campaigns provide valuable datasets to reduce these uncertainties. Here we analyse data from the summer 2014 SWERUS-C3 campaign in the eastern Arctic Ocean, off the shore of Siberia and Alaska. Total concentrations of methane, as well as relative concentrations of 12 CH 4 and 13 CH 4 , were measured continuously during this campaign for 35 d in July and August. Using a chemistry-transport model, we link observed concentrations and isotopic ratios to regional emissions and hemispheric transport structures. A simple inversion system helped constrain source signatures from wetlands in Siberia and Alaska, and oceanic sources, as well as the isotopic composition of lower-stratosphere air masses. The variation in the signature of lower-stratosphere air masses, due to strongly fractionating chemical reactions in the stratosphere, was suggested to explain a large share of the observed variability in isotopic ratios. These results point towards necessary efforts to better simulate large-scale transport and chemistry patterns to make relevant use of isotopic data in remote areas. It is also found that constant and homogeneous source signatures for each type of emission in a given region (mostly wetlands and oil and gas industry in our case at high latitudes) are not compatible with the strong synoptic isotopic signal observed in the Arctic. A regional gradient in source signatures is highlighted between Siberian and Alaskan wetlands, the latter having lighter signatures (more depleted in 13 C). Finally, our results suggest that marine emissions of methane from Arc-tic continental-shelf sources are dominated by thermogenic-origin methane, with a secondary biogenic source as well.
author2 Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Modélisation INVerse pour les mesures atmosphériques et SATellitaires (SATINV)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-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)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
ICOS-RAMCES (ICOS-RAMCES)
Bolin Centre for Climate Research
Stockholm University
This research has been supported by the Franco-Swedish project IZOMET-FS (grant no. VR 2014-6584).
format Article in Journal/Newspaper
author Berchet, Antoine
Pison, Isabelle
Crill, Patrick
Thornton, Brett
Bousquet, Philippe
Thonat, Thibaud
Hocking, Thomas
Thanwerdas, Joël
Paris, Jean-Daniel
Saunois, Marielle
author_facet Berchet, Antoine
Pison, Isabelle
Crill, Patrick
Thornton, Brett
Bousquet, Philippe
Thonat, Thibaud
Hocking, Thomas
Thanwerdas, Joël
Paris, Jean-Daniel
Saunois, Marielle
author_sort Berchet, Antoine
title Using ship-borne observations of methane isotopic ratio in the Arctic Ocean to understand methane sources in the Arctic
title_short Using ship-borne observations of methane isotopic ratio in the Arctic Ocean to understand methane sources in the Arctic
title_full Using ship-borne observations of methane isotopic ratio in the Arctic Ocean to understand methane sources in the Arctic
title_fullStr Using ship-borne observations of methane isotopic ratio in the Arctic Ocean to understand methane sources in the Arctic
title_full_unstemmed Using ship-borne observations of methane isotopic ratio in the Arctic Ocean to understand methane sources in the Arctic
title_sort using ship-borne observations of methane isotopic ratio in the arctic ocean to understand methane sources in the arctic
publisher HAL CCSD
publishDate 2020
url https://hal.archives-ouvertes.fr/hal-02532741
https://hal.archives-ouvertes.fr/hal-02532741/document
https://hal.archives-ouvertes.fr/hal-02532741/file/acp-20-3987-2020.pdf
https://doi.org/10.5194/acp-20-3987-2020
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
SWERUS-C3
Alaska
Siberia
genre_facet Arctic
Arctic Ocean
SWERUS-C3
Alaska
Siberia
op_source ISSN: 1680-7316
EISSN: 1680-7324
Atmospheric Chemistry and Physics
https://hal.archives-ouvertes.fr/hal-02532741
Atmospheric Chemistry and Physics, European Geosciences Union, 2020, 20 (6), pp.3987-3998. ⟨10.5194/acp-20-3987-2020⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/acp-20-3987-2020
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https://hal.archives-ouvertes.fr/hal-02532741
https://hal.archives-ouvertes.fr/hal-02532741/document
https://hal.archives-ouvertes.fr/hal-02532741/file/acp-20-3987-2020.pdf
doi:10.5194/acp-20-3987-2020
op_rights http://creativecommons.org/licenses/by/
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op_doi https://doi.org/10.5194/acp-20-3987-2020
container_title Atmospheric Chemistry and Physics
container_volume 20
container_issue 6
container_start_page 3987
op_container_end_page 3998
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spelling ftccsdartic:oai:HAL:hal-02532741v1 2023-05-15T14:50:10+02:00 Using ship-borne observations of methane isotopic ratio in the Arctic Ocean to understand methane sources in the Arctic Berchet, Antoine Pison, Isabelle Crill, Patrick Thornton, Brett Bousquet, Philippe Thonat, Thibaud Hocking, Thomas Thanwerdas, Joël Paris, Jean-Daniel Saunois, Marielle Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Modélisation INVerse pour les mesures atmosphériques et SATellitaires (SATINV) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-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)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) ICOS-RAMCES (ICOS-RAMCES) Bolin Centre for Climate Research Stockholm University This research has been supported by the Franco-Swedish project IZOMET-FS (grant no. VR 2014-6584). 2020 https://hal.archives-ouvertes.fr/hal-02532741 https://hal.archives-ouvertes.fr/hal-02532741/document https://hal.archives-ouvertes.fr/hal-02532741/file/acp-20-3987-2020.pdf https://doi.org/10.5194/acp-20-3987-2020 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/acp-20-3987-2020 hal-02532741 https://hal.archives-ouvertes.fr/hal-02532741 https://hal.archives-ouvertes.fr/hal-02532741/document https://hal.archives-ouvertes.fr/hal-02532741/file/acp-20-3987-2020.pdf doi:10.5194/acp-20-3987-2020 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 1680-7316 EISSN: 1680-7324 Atmospheric Chemistry and Physics https://hal.archives-ouvertes.fr/hal-02532741 Atmospheric Chemistry and Physics, European Geosciences Union, 2020, 20 (6), pp.3987-3998. ⟨10.5194/acp-20-3987-2020⟩ [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 ftccsdartic https://doi.org/10.5194/acp-20-3987-2020 2021-12-19T00:55:47Z International audience Characterizing methane sources in the Arctic remains challenging due to the remoteness, heterogeneity and variety of such emissions. In situ campaigns provide valuable datasets to reduce these uncertainties. Here we analyse data from the summer 2014 SWERUS-C3 campaign in the eastern Arctic Ocean, off the shore of Siberia and Alaska. Total concentrations of methane, as well as relative concentrations of 12 CH 4 and 13 CH 4 , were measured continuously during this campaign for 35 d in July and August. Using a chemistry-transport model, we link observed concentrations and isotopic ratios to regional emissions and hemispheric transport structures. A simple inversion system helped constrain source signatures from wetlands in Siberia and Alaska, and oceanic sources, as well as the isotopic composition of lower-stratosphere air masses. The variation in the signature of lower-stratosphere air masses, due to strongly fractionating chemical reactions in the stratosphere, was suggested to explain a large share of the observed variability in isotopic ratios. These results point towards necessary efforts to better simulate large-scale transport and chemistry patterns to make relevant use of isotopic data in remote areas. It is also found that constant and homogeneous source signatures for each type of emission in a given region (mostly wetlands and oil and gas industry in our case at high latitudes) are not compatible with the strong synoptic isotopic signal observed in the Arctic. A regional gradient in source signatures is highlighted between Siberian and Alaskan wetlands, the latter having lighter signatures (more depleted in 13 C). Finally, our results suggest that marine emissions of methane from Arc-tic continental-shelf sources are dominated by thermogenic-origin methane, with a secondary biogenic source as well. Article in Journal/Newspaper Arctic Arctic Ocean SWERUS-C3 Alaska Siberia Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Arctic Arctic Ocean Atmospheric Chemistry and Physics 20 6 3987 3998