Blar i Geophysical Institute på emneord "Greenland Sea"
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Continued warming, salinification and oxygenation of the Greenland Sea gyre
(Peer reviewed; Journal article, 2018-06-18)The Greenland Sea gyre is one of the few areas where the water column is ventilated through open ocean convection. This process brings both anthropogenic carbon and oxygen from the atmosphere and surface ocean into the ... -
Deep weakly-stratified layers in the Greenland Sea
(Master thesis, 2021-12-06)Deep weakly-stratified layers in the Greenland Sea constitute a mode of convection poorly understood. The Greenland Sea is where the densest portion of the overflow waters on either side of Iceland are formed through ... -
Intermediate water from the Greenland Sea in the Faroe Bank Channel : spreading of released sulphur hexafluoride
(Journal article, 2005-02)The Faroe Bank Channel is the deepest passage for dense water leaving the Nordic Seas into the North Atlantic. The contribution to this part of the Greenland-Scotland Overflow by intermediate water from the Greenland Sea ...