Ocean convection linked to the recent ice edge retreat along east Greenland

Warm Atlantic water circulates cyclonically around the Nordic Seas while gradually cooling. Here, the authors show that the retreat of the ice edge toward Greenland has led to further transformation of this water mass, which is no longer situated underneath sea ice when transiting the western Icelan...

Description complète

Enregistré dans:

Détails bibliographiques
Auteurs principaux:	Kjetil Våge, Lukas Papritz, Lisbeth Håvik, Michael A. Spall, G. W. K. Moore
Format:	article
Langue:	EN
Publié:	Nature Portfolio 2018
Sujets:	Science Q
Accès en ligne:	https://doaj.org/article/7e30a63ee13046c5ad2fba4ad6f33dce
Tags:	Ajouter un tag Pas de tags, Soyez le premier à ajouter un tag!

id	oai:doaj.org-article:7e30a63ee13046c5ad2fba4ad6f33dce
record_format	dspace
spelling	oai:doaj.org-article:7e30a63ee13046c5ad2fba4ad6f33dce2021-12-02T17:33:02ZOcean convection linked to the recent ice edge retreat along east Greenland10.1038/s41467-018-03468-62041-1723https://doaj.org/article/7e30a63ee13046c5ad2fba4ad6f33dce2018-03-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-03468-6https://doaj.org/toc/2041-1723Warm Atlantic water circulates cyclonically around the Nordic Seas while gradually cooling. Here, the authors show that the retreat of the ice edge toward Greenland has led to further transformation of this water mass, which is no longer situated underneath sea ice when transiting the western Iceland Sea in winter.Kjetil VågeLukas PapritzLisbeth HåvikMichael A. SpallG. W. K. MooreNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-8 (2018)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Kjetil Våge Lukas Papritz Lisbeth Håvik Michael A. Spall G. W. K. Moore Ocean convection linked to the recent ice edge retreat along east Greenland
description	Warm Atlantic water circulates cyclonically around the Nordic Seas while gradually cooling. Here, the authors show that the retreat of the ice edge toward Greenland has led to further transformation of this water mass, which is no longer situated underneath sea ice when transiting the western Iceland Sea in winter.
format	article
author	Kjetil Våge Lukas Papritz Lisbeth Håvik Michael A. Spall G. W. K. Moore
author_facet	Kjetil Våge Lukas Papritz Lisbeth Håvik Michael A. Spall G. W. K. Moore
author_sort	Kjetil Våge
title	Ocean convection linked to the recent ice edge retreat along east Greenland
title_short	Ocean convection linked to the recent ice edge retreat along east Greenland
title_full	Ocean convection linked to the recent ice edge retreat along east Greenland
title_fullStr	Ocean convection linked to the recent ice edge retreat along east Greenland
title_full_unstemmed	Ocean convection linked to the recent ice edge retreat along east Greenland
title_sort	ocean convection linked to the recent ice edge retreat along east greenland
publisher	Nature Portfolio
publishDate	2018
url	https://doaj.org/article/7e30a63ee13046c5ad2fba4ad6f33dce
work_keys_str_mv	AT kjetilvage oceanconvectionlinkedtotherecenticeedgeretreatalongeastgreenland AT lukaspapritz oceanconvectionlinkedtotherecenticeedgeretreatalongeastgreenland AT lisbethhavik oceanconvectionlinkedtotherecenticeedgeretreatalongeastgreenland AT michaelaspall oceanconvectionlinkedtotherecenticeedgeretreatalongeastgreenland AT gwkmoore oceanconvectionlinkedtotherecenticeedgeretreatalongeastgreenland
_version_	1718380070416941056

Ocean convection linked to the recent ice edge retreat along east Greenland

Documents similaires