Increased ventilation of Antarctic deep water during the warm mid-Pliocene
The mid-Pliocene warm period is a recent warm geological period that shares similarities with predictions of future climate. It is generally held the mid-Pliocene Atlantic Meridional Overturning Circulation must have been stronger, to explain a weak Atlantic meridional δ13C gradient and large northe...
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ftpubmed:oai:pubmedcentral.nih.gov:3586712 2023-05-15T14:03:02+02:00 Increased ventilation of Antarctic deep water during the warm mid-Pliocene Zhang, Zhongshi Nisancioglu, Kerim H. Ninnemann, Ulysses S. 2013-02-19 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3586712 http://www.ncbi.nlm.nih.gov/pubmed/23422667 https://doi.org/10.1038/ncomms2521 en eng Nature Pub. Group http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3586712 http://www.ncbi.nlm.nih.gov/pubmed/23422667 http://dx.doi.org/10.1038/ncomms2521 Copyright © 2013, Nature Publishing Group, a division of Macmillan Publishers Limited. All Rights Reserved. http://creativecommons.org/licenses/by-nc-sa/3.0/ This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/3.0/ CC-BY-NC-SA Article Text 2013 ftpubmed https://doi.org/10.1038/ncomms2521 2013-09-04T20:34:36Z The mid-Pliocene warm period is a recent warm geological period that shares similarities with predictions of future climate. It is generally held the mid-Pliocene Atlantic Meridional Overturning Circulation must have been stronger, to explain a weak Atlantic meridional δ13C gradient and large northern high-latitude warming. However, climate models do not simulate such stronger Atlantic Meridional Overturning Circulation, when forced with mid-Pliocene boundary conditions. Proxy reconstructions allow for an alternative scenario that the weak δ13C gradient can be explained by increased ventilation and reduced stratification in the Southern Ocean. Here this alternative scenario is supported by simulations with the Norwegian Earth System Model (NorESM-L), which simulate an intensified and slightly poleward shifted wind field off Antarctica, giving enhanced ventilation and reduced stratification in the Southern Ocean. Our findings challenge the prevailing theory and show how increased Southern Ocean ventilation can reconcile existing model-data discrepancies about Atlantic Meridional Overturning Circulation while explaining fundamental ocean features. Text Antarc* Antarctic Antarctica Southern Ocean PubMed Central (PMC) Antarctic Southern Ocean Nature Communications 4 1 |
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Article Zhang, Zhongshi Nisancioglu, Kerim H. Ninnemann, Ulysses S. Increased ventilation of Antarctic deep water during the warm mid-Pliocene |
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Article |
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The mid-Pliocene warm period is a recent warm geological period that shares similarities with predictions of future climate. It is generally held the mid-Pliocene Atlantic Meridional Overturning Circulation must have been stronger, to explain a weak Atlantic meridional δ13C gradient and large northern high-latitude warming. However, climate models do not simulate such stronger Atlantic Meridional Overturning Circulation, when forced with mid-Pliocene boundary conditions. Proxy reconstructions allow for an alternative scenario that the weak δ13C gradient can be explained by increased ventilation and reduced stratification in the Southern Ocean. Here this alternative scenario is supported by simulations with the Norwegian Earth System Model (NorESM-L), which simulate an intensified and slightly poleward shifted wind field off Antarctica, giving enhanced ventilation and reduced stratification in the Southern Ocean. Our findings challenge the prevailing theory and show how increased Southern Ocean ventilation can reconcile existing model-data discrepancies about Atlantic Meridional Overturning Circulation while explaining fundamental ocean features. |
format |
Text |
author |
Zhang, Zhongshi Nisancioglu, Kerim H. Ninnemann, Ulysses S. |
author_facet |
Zhang, Zhongshi Nisancioglu, Kerim H. Ninnemann, Ulysses S. |
author_sort |
Zhang, Zhongshi |
title |
Increased ventilation of Antarctic deep water during the warm mid-Pliocene |
title_short |
Increased ventilation of Antarctic deep water during the warm mid-Pliocene |
title_full |
Increased ventilation of Antarctic deep water during the warm mid-Pliocene |
title_fullStr |
Increased ventilation of Antarctic deep water during the warm mid-Pliocene |
title_full_unstemmed |
Increased ventilation of Antarctic deep water during the warm mid-Pliocene |
title_sort |
increased ventilation of antarctic deep water during the warm mid-pliocene |
publisher |
Nature Pub. Group |
publishDate |
2013 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3586712 http://www.ncbi.nlm.nih.gov/pubmed/23422667 https://doi.org/10.1038/ncomms2521 |
geographic |
Antarctic Southern Ocean |
geographic_facet |
Antarctic Southern Ocean |
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Antarc* Antarctic Antarctica Southern Ocean |
genre_facet |
Antarc* Antarctic Antarctica Southern Ocean |
op_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3586712 http://www.ncbi.nlm.nih.gov/pubmed/23422667 http://dx.doi.org/10.1038/ncomms2521 |
op_rights |
Copyright © 2013, Nature Publishing Group, a division of Macmillan Publishers Limited. All Rights Reserved. http://creativecommons.org/licenses/by-nc-sa/3.0/ This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/3.0/ |
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CC-BY-NC-SA |
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https://doi.org/10.1038/ncomms2521 |
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Nature Communications |
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4 |
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1 |
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1766273515689869312 |