Mid to late Holocene strengthening of the East Greenland Current linked to warm subsurface Atlantic water

The relatively fresh and cold East Greenland Current (EGC) connects the Arctic with the subpolar North Atlantic Ocean. Its strength and influence on the freshwater balance in the North Atlantic affects both the Subpolar Gyre dynamics and deep convection in the Labrador Sea. Enhanced freshwater and s...

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Bibliographic Details
Published in:Quaternary Science Reviews
Main Authors: Perner, Kerstin, Moros, Matthias, Lloyd, Jeremy M., Jansen, Eystein, Stein, Ruediger
Format: Article in Journal/Newspaper
Language:English
Published: Pergamon-elsevier Science Ltd 2015
Subjects:
Online Access:https://archimer.ifremer.fr/doc/00496/60725/83614.pdf
https://doi.org/10.1016/j.quascirev.2015.10.007
https://archimer.ifremer.fr/doc/00496/60725/