Deep-water circulation changes lead North Atlantic climate during deglaciation

The response time of North Atlantic climate to changes in high-latitude deep-water formation during the last deglaciation is still unclear. Here the authors show that gradual changes in Nordic Seas deep-water circulation systematically lead ahead of abrupt regional climate shifts by ~400 years.

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Autores principales:	Francesco Muschitiello, William J. D’Andrea, Andreas Schmittner, Timothy J. Heaton, Nicholas L. Balascio, Nicole deRoberts, Marc W. Caffee, Thomas E. Woodruff, Kees C. Welten, Luke C. Skinner, Margit H. Simon, Trond M. Dokken
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2019
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/9585679d3e264897aef07f7f7c51c9a0
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spelling	oai:doaj.org-article:9585679d3e264897aef07f7f7c51c9a02021-12-02T15:35:12ZDeep-water circulation changes lead North Atlantic climate during deglaciation10.1038/s41467-019-09237-32041-1723https://doaj.org/article/9585679d3e264897aef07f7f7c51c9a02019-03-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-09237-3https://doaj.org/toc/2041-1723The response time of North Atlantic climate to changes in high-latitude deep-water formation during the last deglaciation is still unclear. Here the authors show that gradual changes in Nordic Seas deep-water circulation systematically lead ahead of abrupt regional climate shifts by ~400 years.Francesco MuschitielloWilliam J. D’AndreaAndreas SchmittnerTimothy J. HeatonNicholas L. BalascioNicole deRobertsMarc W. CaffeeThomas E. WoodruffKees C. WeltenLuke C. SkinnerMargit H. SimonTrond M. DokkenNature PortfolioarticleScienceQENNature Communications, Vol 10, Iss 1, Pp 1-10 (2019)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Francesco Muschitiello William J. D’Andrea Andreas Schmittner Timothy J. Heaton Nicholas L. Balascio Nicole deRoberts Marc W. Caffee Thomas E. Woodruff Kees C. Welten Luke C. Skinner Margit H. Simon Trond M. Dokken Deep-water circulation changes lead North Atlantic climate during deglaciation
description	The response time of North Atlantic climate to changes in high-latitude deep-water formation during the last deglaciation is still unclear. Here the authors show that gradual changes in Nordic Seas deep-water circulation systematically lead ahead of abrupt regional climate shifts by ~400 years.
format	article
author	Francesco Muschitiello William J. D’Andrea Andreas Schmittner Timothy J. Heaton Nicholas L. Balascio Nicole deRoberts Marc W. Caffee Thomas E. Woodruff Kees C. Welten Luke C. Skinner Margit H. Simon Trond M. Dokken
author_facet	Francesco Muschitiello William J. D’Andrea Andreas Schmittner Timothy J. Heaton Nicholas L. Balascio Nicole deRoberts Marc W. Caffee Thomas E. Woodruff Kees C. Welten Luke C. Skinner Margit H. Simon Trond M. Dokken
author_sort	Francesco Muschitiello
title	Deep-water circulation changes lead North Atlantic climate during deglaciation
title_short	Deep-water circulation changes lead North Atlantic climate during deglaciation
title_full	Deep-water circulation changes lead North Atlantic climate during deglaciation
title_fullStr	Deep-water circulation changes lead North Atlantic climate during deglaciation
title_full_unstemmed	Deep-water circulation changes lead North Atlantic climate during deglaciation
title_sort	deep-water circulation changes lead north atlantic climate during deglaciation
publisher	Nature Portfolio
publishDate	2019
url	https://doaj.org/article/9585679d3e264897aef07f7f7c51c9a0
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Deep-water circulation changes lead North Atlantic climate during deglaciation

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