The Dominant Role of Brewer‐Dobson Circulation on 17 O‐Excess Variations in Snow Pits at Dome A, Antarctica
International audience Previous studies have shown that the mass-independent fractionation of oxygen isotope (O-MIF) in the atmosphere can occur during photochemical reactions of ozone (
Published in: | Journal of Geophysical Research: Atmospheres |
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HAL CCSD
2022
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Online Access: | https://hal.science/hal-03738524 https://hal.science/hal-03738524/document https://hal.science/hal-03738524/file/JGR%20Atmospheres%20-%202022%20-%20Pang%20-%20The%20Dominant%20Role%20of%20Brewer%25E2%2580%2590Dobson%20Circulation%20on%2017O%25E2%2580%2590Excess%20Variations%20in%20Snow%20Pits%20at.pdf https://doi.org/10.1029/2022jd036559 |
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ftinsu:oai:HAL:hal-03738524v1 2024-04-28T08:00:58+00:00 The Dominant Role of Brewer‐Dobson Circulation on 17 O‐Excess Variations in Snow Pits at Dome A, Antarctica Pang, Hongxi Zhang, Peng Wu, Shuangye Jouzel, Jean Steen‐larsen, Hans, Christian Liu, Ke Zhang, Wangbin Yu, Jinhai An, Chunlei Chen, Deliang Hou, Shugui Nanjing University (NJU) Göteborgs Universitet = University of Gothenburg (GU) University of Dayton 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) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) 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)) University of Bergen (UiB) Polar Research Institute of China (PRIC) We thank all of the CHINARE-26 and CHINARE-32 scientists, technicians, and porters for their hard work in the field. We thank Amaelle Landais (LSCE) for the 17O-excess measurements and her constructive comments on this paper. We also thank Tongmei Wang for her advice on calculating the residual circulation. This work was jointly supported by the National Natural Science Foundation of China (41622605, 41830644, 91837102, 42021001), the Chinese Arctic and Antarctic Administration (CXPT2020012), the Priority Academic Program Development of Jiangsu Higher Education Institutions (PAPD), and the Swedish STINT (CH2019-8377). 2022-07-05 https://hal.science/hal-03738524 https://hal.science/hal-03738524/document https://hal.science/hal-03738524/file/JGR%20Atmospheres%20-%202022%20-%20Pang%20-%20The%20Dominant%20Role%20of%20Brewer%25E2%2580%2590Dobson%20Circulation%20on%2017O%25E2%2580%2590Excess%20Variations%20in%20Snow%20Pits%20at.pdf https://doi.org/10.1029/2022jd036559 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2022jd036559 hal-03738524 https://hal.science/hal-03738524 https://hal.science/hal-03738524/document https://hal.science/hal-03738524/file/JGR%20Atmospheres%20-%202022%20-%20Pang%20-%20The%20Dominant%20Role%20of%20Brewer%25E2%2580%2590Dobson%20Circulation%20on%2017O%25E2%2580%2590Excess%20Variations%20in%20Snow%20Pits%20at.pdf doi:10.1029/2022jd036559 info:eu-repo/semantics/OpenAccess ISSN: 2169-897X EISSN: 2169-8996 Journal of Geophysical Research: Atmospheres https://hal.science/hal-03738524 Journal of Geophysical Research: Atmospheres, 2022, 127 (13), pp.e2022JD036559. ⟨10.1029/2022jd036559⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2022 ftinsu https://doi.org/10.1029/2022jd036559 2024-04-05T00:32:43Z International audience Previous studies have shown that the mass-independent fractionation of oxygen isotope (O-MIF) in the atmosphere can occur during photochemical reactions of ozone ( Article in Journal/Newspaper Antarc* Antarctica Institut national des sciences de l'Univers: HAL-INSU Journal of Geophysical Research: Atmospheres 127 13 |
institution |
Open Polar |
collection |
Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
spellingShingle |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment Pang, Hongxi Zhang, Peng Wu, Shuangye Jouzel, Jean Steen‐larsen, Hans, Christian Liu, Ke Zhang, Wangbin Yu, Jinhai An, Chunlei Chen, Deliang Hou, Shugui The Dominant Role of Brewer‐Dobson Circulation on 17 O‐Excess Variations in Snow Pits at Dome A, Antarctica |
topic_facet |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
description |
International audience Previous studies have shown that the mass-independent fractionation of oxygen isotope (O-MIF) in the atmosphere can occur during photochemical reactions of ozone ( |
author2 |
Nanjing University (NJU) Göteborgs Universitet = University of Gothenburg (GU) University of Dayton 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) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) 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)) University of Bergen (UiB) Polar Research Institute of China (PRIC) We thank all of the CHINARE-26 and CHINARE-32 scientists, technicians, and porters for their hard work in the field. We thank Amaelle Landais (LSCE) for the 17O-excess measurements and her constructive comments on this paper. We also thank Tongmei Wang for her advice on calculating the residual circulation. This work was jointly supported by the National Natural Science Foundation of China (41622605, 41830644, 91837102, 42021001), the Chinese Arctic and Antarctic Administration (CXPT2020012), the Priority Academic Program Development of Jiangsu Higher Education Institutions (PAPD), and the Swedish STINT (CH2019-8377). |
format |
Article in Journal/Newspaper |
author |
Pang, Hongxi Zhang, Peng Wu, Shuangye Jouzel, Jean Steen‐larsen, Hans, Christian Liu, Ke Zhang, Wangbin Yu, Jinhai An, Chunlei Chen, Deliang Hou, Shugui |
author_facet |
Pang, Hongxi Zhang, Peng Wu, Shuangye Jouzel, Jean Steen‐larsen, Hans, Christian Liu, Ke Zhang, Wangbin Yu, Jinhai An, Chunlei Chen, Deliang Hou, Shugui |
author_sort |
Pang, Hongxi |
title |
The Dominant Role of Brewer‐Dobson Circulation on 17 O‐Excess Variations in Snow Pits at Dome A, Antarctica |
title_short |
The Dominant Role of Brewer‐Dobson Circulation on 17 O‐Excess Variations in Snow Pits at Dome A, Antarctica |
title_full |
The Dominant Role of Brewer‐Dobson Circulation on 17 O‐Excess Variations in Snow Pits at Dome A, Antarctica |
title_fullStr |
The Dominant Role of Brewer‐Dobson Circulation on 17 O‐Excess Variations in Snow Pits at Dome A, Antarctica |
title_full_unstemmed |
The Dominant Role of Brewer‐Dobson Circulation on 17 O‐Excess Variations in Snow Pits at Dome A, Antarctica |
title_sort |
dominant role of brewer‐dobson circulation on 17 o‐excess variations in snow pits at dome a, antarctica |
publisher |
HAL CCSD |
publishDate |
2022 |
url |
https://hal.science/hal-03738524 https://hal.science/hal-03738524/document https://hal.science/hal-03738524/file/JGR%20Atmospheres%20-%202022%20-%20Pang%20-%20The%20Dominant%20Role%20of%20Brewer%25E2%2580%2590Dobson%20Circulation%20on%2017O%25E2%2580%2590Excess%20Variations%20in%20Snow%20Pits%20at.pdf https://doi.org/10.1029/2022jd036559 |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
ISSN: 2169-897X EISSN: 2169-8996 Journal of Geophysical Research: Atmospheres https://hal.science/hal-03738524 Journal of Geophysical Research: Atmospheres, 2022, 127 (13), pp.e2022JD036559. ⟨10.1029/2022jd036559⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2022jd036559 hal-03738524 https://hal.science/hal-03738524 https://hal.science/hal-03738524/document https://hal.science/hal-03738524/file/JGR%20Atmospheres%20-%202022%20-%20Pang%20-%20The%20Dominant%20Role%20of%20Brewer%25E2%2580%2590Dobson%20Circulation%20on%2017O%25E2%2580%2590Excess%20Variations%20in%20Snow%20Pits%20at.pdf doi:10.1029/2022jd036559 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1029/2022jd036559 |
container_title |
Journal of Geophysical Research: Atmospheres |
container_volume |
127 |
container_issue |
13 |
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1797572937719480320 |