Mechanisms of Global Ocean Ventilation Age Change during the Last Deglaciation
Marine radiocarbon (14C) is widely used to trace deep ocean circulation, providing insight into the atmosphere-ocean exchange of CO2 during the last deglaciation. Using two transient simulations with tracers of 14C and ideal age, we found that the oldest ventilation age is not observed at the Last G...
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Copernicus Publications
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00069206 2023-11-12T04:03:06+01:00 Mechanisms of Global Ocean Ventilation Age Change during the Last Deglaciation Li, Lingwei Liu, Zhengyu Du, Jinbo Wan, Lingfeng Lu, Jiuyou 2023-10 electronic https://doi.org/10.5194/egusphere-2023-2256 https://noa.gwlb.de/receive/cop_mods_00069206 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00067603/egusphere-2023-2256.pdf https://egusphere.copernicus.org/preprints/2023/egusphere-2023-2256/egusphere-2023-2256.pdf eng eng Copernicus Publications https://doi.org/10.5194/egusphere-2023-2256 https://noa.gwlb.de/receive/cop_mods_00069206 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00067603/egusphere-2023-2256.pdf https://egusphere.copernicus.org/preprints/2023/egusphere-2023-2256/egusphere-2023-2256.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2023 ftnonlinearchiv https://doi.org/10.5194/egusphere-2023-2256 2023-10-15T23:22:18Z Marine radiocarbon (14C) is widely used to trace deep ocean circulation, providing insight into the atmosphere-ocean exchange of CO2 during the last deglaciation. Using two transient simulations with tracers of 14C and ideal age, we found that the oldest ventilation age is not observed at the Last Glacial Maximum (LGM). In contrast, the model shows a modestly younger ventilation age during the LGM compared to present day, mainly due to a stronger glacial Antarctic Bottom Water (AABW) transport associated with sea ice expansion. Notably, the ocean ventilation age is significantly older around 14–12 ka compared to the age at the LGM, with deep Pacific waters playing a predominant role, primarily caused by the weakening of AABW transport. Article in Journal/Newspaper Antarc* Antarctic Sea ice Niedersächsisches Online-Archiv NOA Antarctic Pacific |
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Niedersächsisches Online-Archiv NOA |
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ftnonlinearchiv |
language |
English |
topic |
article Verlagsveröffentlichung |
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article Verlagsveröffentlichung Li, Lingwei Liu, Zhengyu Du, Jinbo Wan, Lingfeng Lu, Jiuyou Mechanisms of Global Ocean Ventilation Age Change during the Last Deglaciation |
topic_facet |
article Verlagsveröffentlichung |
description |
Marine radiocarbon (14C) is widely used to trace deep ocean circulation, providing insight into the atmosphere-ocean exchange of CO2 during the last deglaciation. Using two transient simulations with tracers of 14C and ideal age, we found that the oldest ventilation age is not observed at the Last Glacial Maximum (LGM). In contrast, the model shows a modestly younger ventilation age during the LGM compared to present day, mainly due to a stronger glacial Antarctic Bottom Water (AABW) transport associated with sea ice expansion. Notably, the ocean ventilation age is significantly older around 14–12 ka compared to the age at the LGM, with deep Pacific waters playing a predominant role, primarily caused by the weakening of AABW transport. |
format |
Article in Journal/Newspaper |
author |
Li, Lingwei Liu, Zhengyu Du, Jinbo Wan, Lingfeng Lu, Jiuyou |
author_facet |
Li, Lingwei Liu, Zhengyu Du, Jinbo Wan, Lingfeng Lu, Jiuyou |
author_sort |
Li, Lingwei |
title |
Mechanisms of Global Ocean Ventilation Age Change during the Last Deglaciation |
title_short |
Mechanisms of Global Ocean Ventilation Age Change during the Last Deglaciation |
title_full |
Mechanisms of Global Ocean Ventilation Age Change during the Last Deglaciation |
title_fullStr |
Mechanisms of Global Ocean Ventilation Age Change during the Last Deglaciation |
title_full_unstemmed |
Mechanisms of Global Ocean Ventilation Age Change during the Last Deglaciation |
title_sort |
mechanisms of global ocean ventilation age change during the last deglaciation |
publisher |
Copernicus Publications |
publishDate |
2023 |
url |
https://doi.org/10.5194/egusphere-2023-2256 https://noa.gwlb.de/receive/cop_mods_00069206 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00067603/egusphere-2023-2256.pdf https://egusphere.copernicus.org/preprints/2023/egusphere-2023-2256/egusphere-2023-2256.pdf |
geographic |
Antarctic Pacific |
geographic_facet |
Antarctic Pacific |
genre |
Antarc* Antarctic Sea ice |
genre_facet |
Antarc* Antarctic Sea ice |
op_relation |
https://doi.org/10.5194/egusphere-2023-2256 https://noa.gwlb.de/receive/cop_mods_00069206 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00067603/egusphere-2023-2256.pdf https://egusphere.copernicus.org/preprints/2023/egusphere-2023-2256/egusphere-2023-2256.pdf |
op_rights |
https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/egusphere-2023-2256 |
_version_ |
1782336129800863744 |