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...

Full description

Bibliographic Details
Published in:Quaternary Science Reviews
Main Authors: Perner, Kerstin, Moros, Matthias, Lloyd, Jeremy M., Jansen, Eystein, Stein, Ruediger
Format: Text
Language:English
Published: Pergamon-elsevier Science Ltd
Subjects:
envir
geo
Arctic
Arctic Ocean
Foster Bugt
Greenland
East Greenland
east greenland current
Foraminifera*
Foster bugt
Labrador Sea
north atlantic current
North Atlantic
Sea ice
Spitsbergen
Online Access:https://doi.org/10.1016/j.quascirev.2015.10.007
https://archimer.ifremer.fr/doc/00496/60725/83614.pdf
https://archimer.ifremer.fr/doc/00496/60725/

Similar Items