Threshold in North Atlantic-Arctic Ocean circulation controlled by the subsidence of the Greenland-Scotland Ridge

During the Cenozoic the Arctic Ocean change from a restricted freshwater regime towards more saline modern ocean conditions is supposedly driven by the subsidence of the Greenland-Scotland Ridge. Here, the authors derive a threshold for this shift, constrained by the characteristic depth of wind mix...

Descripción completa

Guardado en:

Detalles Bibliográficos
Autores principales:	Michael Stärz, Wilfried Jokat, Gregor Knorr, Gerrit Lohmann
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2017
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/1103bd41c46b4f20850c6be39cb5e77e
Etiquetas:	Agregar Etiqueta Sin Etiquetas, Sea el primero en etiquetar este registro!

id	oai:doaj.org-article:1103bd41c46b4f20850c6be39cb5e77e
record_format	dspace
spelling	oai:doaj.org-article:1103bd41c46b4f20850c6be39cb5e77e2021-12-02T15:38:54ZThreshold in North Atlantic-Arctic Ocean circulation controlled by the subsidence of the Greenland-Scotland Ridge10.1038/ncomms156812041-1723https://doaj.org/article/1103bd41c46b4f20850c6be39cb5e77e2017-06-01T00:00:00Zhttps://doi.org/10.1038/ncomms15681https://doaj.org/toc/2041-1723During the Cenozoic the Arctic Ocean change from a restricted freshwater regime towards more saline modern ocean conditions is supposedly driven by the subsidence of the Greenland-Scotland Ridge. Here, the authors derive a threshold for this shift, constrained by the characteristic depth of wind mixing.Michael StärzWilfried JokatGregor KnorrGerrit LohmannNature PortfolioarticleScienceQENNature Communications, Vol 8, Iss 1, Pp 1-13 (2017)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Michael Stärz Wilfried Jokat Gregor Knorr Gerrit Lohmann Threshold in North Atlantic-Arctic Ocean circulation controlled by the subsidence of the Greenland-Scotland Ridge
description	During the Cenozoic the Arctic Ocean change from a restricted freshwater regime towards more saline modern ocean conditions is supposedly driven by the subsidence of the Greenland-Scotland Ridge. Here, the authors derive a threshold for this shift, constrained by the characteristic depth of wind mixing.
format	article
author	Michael Stärz Wilfried Jokat Gregor Knorr Gerrit Lohmann
author_facet	Michael Stärz Wilfried Jokat Gregor Knorr Gerrit Lohmann
author_sort	Michael Stärz
title	Threshold in North Atlantic-Arctic Ocean circulation controlled by the subsidence of the Greenland-Scotland Ridge
title_short	Threshold in North Atlantic-Arctic Ocean circulation controlled by the subsidence of the Greenland-Scotland Ridge
title_full	Threshold in North Atlantic-Arctic Ocean circulation controlled by the subsidence of the Greenland-Scotland Ridge
title_fullStr	Threshold in North Atlantic-Arctic Ocean circulation controlled by the subsidence of the Greenland-Scotland Ridge
title_full_unstemmed	Threshold in North Atlantic-Arctic Ocean circulation controlled by the subsidence of the Greenland-Scotland Ridge
title_sort	threshold in north atlantic-arctic ocean circulation controlled by the subsidence of the greenland-scotland ridge
publisher	Nature Portfolio
publishDate	2017
url	https://doaj.org/article/1103bd41c46b4f20850c6be39cb5e77e
work_keys_str_mv	AT michaelstarz thresholdinnorthatlanticarcticoceancirculationcontrolledbythesubsidenceofthegreenlandscotlandridge AT wilfriedjokat thresholdinnorthatlanticarcticoceancirculationcontrolledbythesubsidenceofthegreenlandscotlandridge AT gregorknorr thresholdinnorthatlanticarcticoceancirculationcontrolledbythesubsidenceofthegreenlandscotlandridge AT gerritlohmann thresholdinnorthatlanticarcticoceancirculationcontrolledbythesubsidenceofthegreenlandscotlandridge
_version_	1718386034559942656

Threshold in North Atlantic-Arctic Ocean circulation controlled by the subsidence of the Greenland-Scotland Ridge

Ejemplares similares