Modelled ocean changes at the Plio-Pleistocene transition driven by Antarctic ice advance

Global deep water mass properties converged in the North Pacific and Atlantic oceans during the Pliocene-Pleistocene. Here, using a coupled ocean-atmosphere climate model, the authors show that a reduction in coastal ice in the Pacific sector of Antarctica was likely responsible for this change.

Bibliographic Details
Published in:Nature Communications
Main Authors: Daniel J. Hill, Kevin P. Bolton, Alan M. Haywood
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2017
Subjects:
Science
Q
Antarctic
Pacific
Antarc*
Antarctica
Online Access:https://doi.org/10.1038/ncomms14376
https://doaj.org/article/2587fadd10274af0beb6019ae4400086
id ftdoajarticles:oai:doaj.org/article:2587fadd10274af0beb6019ae4400086
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spelling ftdoajarticles:oai:doaj.org/article:2587fadd10274af0beb6019ae4400086 2023-05-15T13:48:04+02:00 Modelled ocean changes at the Plio-Pleistocene transition driven by Antarctic ice advance Daniel J. Hill Kevin P. Bolton Alan M. Haywood 2017-03-01T00:00:00Z https://doi.org/10.1038/ncomms14376 https://doaj.org/article/2587fadd10274af0beb6019ae4400086 EN eng Nature Portfolio https://doi.org/10.1038/ncomms14376 https://doaj.org/toc/2041-1723 doi:10.1038/ncomms14376 2041-1723 https://doaj.org/article/2587fadd10274af0beb6019ae4400086 Nature Communications, Vol 8, Iss 1, Pp 1-8 (2017) Science Q article 2017 ftdoajarticles https://doi.org/10.1038/ncomms14376 2022-12-31T04:18:23Z Global deep water mass properties converged in the North Pacific and Atlantic oceans during the Pliocene-Pleistocene. Here, using a coupled ocean-atmosphere climate model, the authors show that a reduction in coastal ice in the Pacific sector of Antarctica was likely responsible for this change. Article in Journal/Newspaper Antarc* Antarctic Antarctica Directory of Open Access Journals: DOAJ Articles Antarctic Pacific Nature Communications 8 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
spellingShingle Science
Q
Daniel J. Hill
Kevin P. Bolton
Alan M. Haywood
Modelled ocean changes at the Plio-Pleistocene transition driven by Antarctic ice advance
topic_facet Science
Q
description Global deep water mass properties converged in the North Pacific and Atlantic oceans during the Pliocene-Pleistocene. Here, using a coupled ocean-atmosphere climate model, the authors show that a reduction in coastal ice in the Pacific sector of Antarctica was likely responsible for this change.
format Article in Journal/Newspaper
author Daniel J. Hill
Kevin P. Bolton
Alan M. Haywood
author_facet Daniel J. Hill
Kevin P. Bolton
Alan M. Haywood
author_sort Daniel J. Hill
title Modelled ocean changes at the Plio-Pleistocene transition driven by Antarctic ice advance
title_short Modelled ocean changes at the Plio-Pleistocene transition driven by Antarctic ice advance
title_full Modelled ocean changes at the Plio-Pleistocene transition driven by Antarctic ice advance
title_fullStr Modelled ocean changes at the Plio-Pleistocene transition driven by Antarctic ice advance
title_full_unstemmed Modelled ocean changes at the Plio-Pleistocene transition driven by Antarctic ice advance
title_sort modelled ocean changes at the plio-pleistocene transition driven by antarctic ice advance
publisher Nature Portfolio
publishDate 2017
url https://doi.org/10.1038/ncomms14376
https://doaj.org/article/2587fadd10274af0beb6019ae4400086
geographic Antarctic
Pacific
geographic_facet Antarctic
Pacific
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_source Nature Communications, Vol 8, Iss 1, Pp 1-8 (2017)
op_relation https://doi.org/10.1038/ncomms14376
https://doaj.org/toc/2041-1723
doi:10.1038/ncomms14376
2041-1723
https://doaj.org/article/2587fadd10274af0beb6019ae4400086
op_doi https://doi.org/10.1038/ncomms14376
container_title Nature Communications
container_volume 8
container_issue 1
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