Dust and sea salt variability in central East Antarctica (Dome C) over the last 45 kyrs and its implications for southern high-latitude climate
International audience A detailed record of non-sea-salt calcium, a proxy for dust, and sea-salt sodium, a proxy for sea salt, covering the last 45 kyr is presented. It shows that in the first part of the transition from the last glacial period to the Holocene (18-15 kyr BP), the changes in dust flu...
Published in: | Geophysical Research Letters |
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Format: | Article in Journal/Newspaper |
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Online Access: | https://hal.archives-ouvertes.fr/hal-03110023 https://hal.archives-ouvertes.fr/hal-03110023/document https://hal.archives-ouvertes.fr/hal-03110023/file/2002GL015186.pdf https://doi.org/10.1029/2002GL015186 |
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ftccsdartic:oai:HAL:hal-03110023v1 2023-05-15T13:48:19+02:00 Dust and sea salt variability in central East Antarctica (Dome C) over the last 45 kyrs and its implications for southern high-latitude climate Röthlisberger, Regine Mulvaney, Robert Wolff, Eric Hutterli, Manuel Bigler, Matthias Sommer, Stefan Jouzel, Jean British Antarctic Survey (BAS) Natural Environment Research Council (NERC) Climate and Environmental Physics Bern (CEP) Physikalisches Institut Bern Universität Bern Bern -Universität Bern Bern Department of Hydrology and Water Resources (HWR) University of Arizona 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) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) 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) 2002-10 https://hal.archives-ouvertes.fr/hal-03110023 https://hal.archives-ouvertes.fr/hal-03110023/document https://hal.archives-ouvertes.fr/hal-03110023/file/2002GL015186.pdf https://doi.org/10.1029/2002GL015186 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2002GL015186 hal-03110023 https://hal.archives-ouvertes.fr/hal-03110023 https://hal.archives-ouvertes.fr/hal-03110023/document https://hal.archives-ouvertes.fr/hal-03110023/file/2002GL015186.pdf doi:10.1029/2002GL015186 info:eu-repo/semantics/OpenAccess ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal.archives-ouvertes.fr/hal-03110023 Geophysical Research Letters, American Geophysical Union, 2002, 29 (20), pp.24-1-24-4. ⟨10.1029/2002GL015186⟩ [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 2002 ftccsdartic https://doi.org/10.1029/2002GL015186 2021-12-19T00:30:37Z International audience A detailed record of non-sea-salt calcium, a proxy for dust, and sea-salt sodium, a proxy for sea salt, covering the last 45 kyr is presented. It shows that in the first part of the transition from the last glacial period to the Holocene (18-15 kyr BP), the changes in dust flux mainly reflect changes at the dust source, namely vegetation cover and local climate. The changes in the later part of the transition (12-11 kyr BP) are similar in extent to the changes seen in sea salt and most likely reflect a reorganization of the atmospheric circulation. During the last glacial period, considerable variation of dust but not of sea salt is observed, pointing to climatic changes in Patagonia, the main dust source for Dome C. A comparison of the glacial records from Dome C and Taylor Dome suggests that similar influences controlled aerosol input at both sites during this period. Article in Journal/Newspaper Antarc* Antarctica East Antarctica Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) East Antarctica Patagonia Taylor Dome ENVELOPE(157.667,157.667,-77.667,-77.667) Geophysical Research Letters 29 20 24-1 24-4 |
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.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 Röthlisberger, Regine Mulvaney, Robert Wolff, Eric Hutterli, Manuel Bigler, Matthias Sommer, Stefan Jouzel, Jean Dust and sea salt variability in central East Antarctica (Dome C) over the last 45 kyrs and its implications for southern high-latitude climate |
topic_facet |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
description |
International audience A detailed record of non-sea-salt calcium, a proxy for dust, and sea-salt sodium, a proxy for sea salt, covering the last 45 kyr is presented. It shows that in the first part of the transition from the last glacial period to the Holocene (18-15 kyr BP), the changes in dust flux mainly reflect changes at the dust source, namely vegetation cover and local climate. The changes in the later part of the transition (12-11 kyr BP) are similar in extent to the changes seen in sea salt and most likely reflect a reorganization of the atmospheric circulation. During the last glacial period, considerable variation of dust but not of sea salt is observed, pointing to climatic changes in Patagonia, the main dust source for Dome C. A comparison of the glacial records from Dome C and Taylor Dome suggests that similar influences controlled aerosol input at both sites during this period. |
author2 |
British Antarctic Survey (BAS) Natural Environment Research Council (NERC) Climate and Environmental Physics Bern (CEP) Physikalisches Institut Bern Universität Bern Bern -Universität Bern Bern Department of Hydrology and Water Resources (HWR) University of Arizona 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) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) 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) |
format |
Article in Journal/Newspaper |
author |
Röthlisberger, Regine Mulvaney, Robert Wolff, Eric Hutterli, Manuel Bigler, Matthias Sommer, Stefan Jouzel, Jean |
author_facet |
Röthlisberger, Regine Mulvaney, Robert Wolff, Eric Hutterli, Manuel Bigler, Matthias Sommer, Stefan Jouzel, Jean |
author_sort |
Röthlisberger, Regine |
title |
Dust and sea salt variability in central East Antarctica (Dome C) over the last 45 kyrs and its implications for southern high-latitude climate |
title_short |
Dust and sea salt variability in central East Antarctica (Dome C) over the last 45 kyrs and its implications for southern high-latitude climate |
title_full |
Dust and sea salt variability in central East Antarctica (Dome C) over the last 45 kyrs and its implications for southern high-latitude climate |
title_fullStr |
Dust and sea salt variability in central East Antarctica (Dome C) over the last 45 kyrs and its implications for southern high-latitude climate |
title_full_unstemmed |
Dust and sea salt variability in central East Antarctica (Dome C) over the last 45 kyrs and its implications for southern high-latitude climate |
title_sort |
dust and sea salt variability in central east antarctica (dome c) over the last 45 kyrs and its implications for southern high-latitude climate |
publisher |
HAL CCSD |
publishDate |
2002 |
url |
https://hal.archives-ouvertes.fr/hal-03110023 https://hal.archives-ouvertes.fr/hal-03110023/document https://hal.archives-ouvertes.fr/hal-03110023/file/2002GL015186.pdf https://doi.org/10.1029/2002GL015186 |
long_lat |
ENVELOPE(157.667,157.667,-77.667,-77.667) |
geographic |
East Antarctica Patagonia Taylor Dome |
geographic_facet |
East Antarctica Patagonia Taylor Dome |
genre |
Antarc* Antarctica East Antarctica |
genre_facet |
Antarc* Antarctica East Antarctica |
op_source |
ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal.archives-ouvertes.fr/hal-03110023 Geophysical Research Letters, American Geophysical Union, 2002, 29 (20), pp.24-1-24-4. ⟨10.1029/2002GL015186⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2002GL015186 hal-03110023 https://hal.archives-ouvertes.fr/hal-03110023 https://hal.archives-ouvertes.fr/hal-03110023/document https://hal.archives-ouvertes.fr/hal-03110023/file/2002GL015186.pdf doi:10.1029/2002GL015186 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1029/2002GL015186 |
container_title |
Geophysical Research Letters |
container_volume |
29 |
container_issue |
20 |
container_start_page |
24-1 |
op_container_end_page |
24-4 |
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1766249091292987392 |