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...

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Autores principales: Kjetil Våge, Lukas Papritz, Lisbeth Håvik, Michael A. Spall, G. W. K. Moore
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2018
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Acceso en línea:https://doaj.org/article/7e30a63ee13046c5ad2fba4ad6f33dce
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