Early Eocene vigorous ocean overturning and its contribution to a warm Southern Ocean
The early Eocene (~ 55 Ma) is the warmest period, and most likely characterized by the highest atmospheric CO 2 concentrations, of the Cenozoic era. Here, we analyze simulations of the early Eocene performed with the IPSL-CM5A2 coupled climate model set up with paleogeographic reconstructions of thi...
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ftcopernicus:oai:publications.copernicus.org:cpd82541 2023-05-15T13:55:27+02:00 Early Eocene vigorous ocean overturning and its contribution to a warm Southern Ocean Zhang, Yurui Huck, Thierry Lique, Camille Donnadieu, Yannick Ladant, Jean-Baptiste Rabineau, Marina Aslanian, Daniel 2020-01-16 application/pdf https://doi.org/10.5194/cp-2019-163 https://www.clim-past-discuss.net/cp-2019-163/ eng eng doi:10.5194/cp-2019-163 https://www.clim-past-discuss.net/cp-2019-163/ eISSN: 1814-9332 Text 2020 ftcopernicus https://doi.org/10.5194/cp-2019-163 2020-01-20T15:41:59Z The early Eocene (~ 55 Ma) is the warmest period, and most likely characterized by the highest atmospheric CO 2 concentrations, of the Cenozoic era. Here, we analyze simulations of the early Eocene performed with the IPSL-CM5A2 coupled climate model set up with paleogeographic reconstructions of this period from the DeepMIP project, with different levels of atmospheric CO 2 , and compare them with simulations of the modern conditions. This allows us to explore the changes of the ocean circulation and the resulting ocean meridional heat transport. At a CO 2 level of 840 ppm, the Early Eocene simulation is characterized by a strong abyssal overturning circulation in the Southern Hemisphere (40 Sv at 60º S), fed by deep water formation in the three sectors of the Southern Ocean. Deep convection in the Southern Ocean is favored by the closed Drake and Tasmanian passages, which provide western boundaries for the build-up of strong subpolar gyres in the Weddell and Ross seas, in the middle of which convection develops. The strong overturning circulation, associated with the subpolar gyres, sustains the poleward advection of saline subtropical water to the convective region in the Southern Ocean, maintaining deep-water formation. This salt-advection feedback mechanism works similarly in the present-day North Atlantic overturning circulation. The strong abyssal overturning circulation in the 55 Ma simulations primarily results in an enhanced poleward ocean heat transport by 0.3–0.7 PW in the Southern Hemisphere compared to modern conditions, reaching 1.7 PW southward at 20° S, and contributing to maintain the Southern Ocean and Antarctica warm in the Eocene. Simulations with different atmospheric CO 2 levels show that the ocean circulation and heat transport are relatively insensitive to CO 2 -doubling. Text Antarc* Antarctica North Atlantic Southern Ocean Copernicus Publications: E-Journals Southern Ocean Weddell |
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Copernicus Publications: E-Journals |
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ftcopernicus |
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English |
description |
The early Eocene (~ 55 Ma) is the warmest period, and most likely characterized by the highest atmospheric CO 2 concentrations, of the Cenozoic era. Here, we analyze simulations of the early Eocene performed with the IPSL-CM5A2 coupled climate model set up with paleogeographic reconstructions of this period from the DeepMIP project, with different levels of atmospheric CO 2 , and compare them with simulations of the modern conditions. This allows us to explore the changes of the ocean circulation and the resulting ocean meridional heat transport. At a CO 2 level of 840 ppm, the Early Eocene simulation is characterized by a strong abyssal overturning circulation in the Southern Hemisphere (40 Sv at 60º S), fed by deep water formation in the three sectors of the Southern Ocean. Deep convection in the Southern Ocean is favored by the closed Drake and Tasmanian passages, which provide western boundaries for the build-up of strong subpolar gyres in the Weddell and Ross seas, in the middle of which convection develops. The strong overturning circulation, associated with the subpolar gyres, sustains the poleward advection of saline subtropical water to the convective region in the Southern Ocean, maintaining deep-water formation. This salt-advection feedback mechanism works similarly in the present-day North Atlantic overturning circulation. The strong abyssal overturning circulation in the 55 Ma simulations primarily results in an enhanced poleward ocean heat transport by 0.3–0.7 PW in the Southern Hemisphere compared to modern conditions, reaching 1.7 PW southward at 20° S, and contributing to maintain the Southern Ocean and Antarctica warm in the Eocene. Simulations with different atmospheric CO 2 levels show that the ocean circulation and heat transport are relatively insensitive to CO 2 -doubling. |
format |
Text |
author |
Zhang, Yurui Huck, Thierry Lique, Camille Donnadieu, Yannick Ladant, Jean-Baptiste Rabineau, Marina Aslanian, Daniel |
spellingShingle |
Zhang, Yurui Huck, Thierry Lique, Camille Donnadieu, Yannick Ladant, Jean-Baptiste Rabineau, Marina Aslanian, Daniel Early Eocene vigorous ocean overturning and its contribution to a warm Southern Ocean |
author_facet |
Zhang, Yurui Huck, Thierry Lique, Camille Donnadieu, Yannick Ladant, Jean-Baptiste Rabineau, Marina Aslanian, Daniel |
author_sort |
Zhang, Yurui |
title |
Early Eocene vigorous ocean overturning and its contribution to a warm Southern Ocean |
title_short |
Early Eocene vigorous ocean overturning and its contribution to a warm Southern Ocean |
title_full |
Early Eocene vigorous ocean overturning and its contribution to a warm Southern Ocean |
title_fullStr |
Early Eocene vigorous ocean overturning and its contribution to a warm Southern Ocean |
title_full_unstemmed |
Early Eocene vigorous ocean overturning and its contribution to a warm Southern Ocean |
title_sort |
early eocene vigorous ocean overturning and its contribution to a warm southern ocean |
publishDate |
2020 |
url |
https://doi.org/10.5194/cp-2019-163 https://www.clim-past-discuss.net/cp-2019-163/ |
geographic |
Southern Ocean Weddell |
geographic_facet |
Southern Ocean Weddell |
genre |
Antarc* Antarctica North Atlantic Southern Ocean |
genre_facet |
Antarc* Antarctica North Atlantic Southern Ocean |
op_source |
eISSN: 1814-9332 |
op_relation |
doi:10.5194/cp-2019-163 https://www.clim-past-discuss.net/cp-2019-163/ |
op_doi |
https://doi.org/10.5194/cp-2019-163 |
_version_ |
1766262076103196672 |