Articles | Volume 12, issue 6
https://doi.org/10.5194/os-12-1205-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/os-12-1205-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
A stable Faroe Bank Channel overflow 1995–2015
Bogi Hansen
CORRESPONDING AUTHOR
Faroe Marine Research Institute, P.O. Box 3051, 110 Tórshavn,
Faroe Islands
Karin Margretha Húsgarð Larsen
Faroe Marine Research Institute, P.O. Box 3051, 110 Tórshavn,
Faroe Islands
Hjálmar Hátún
Faroe Marine Research Institute, P.O. Box 3051, 110 Tórshavn,
Faroe Islands
Svein Østerhus
Uni Research Climate, Nygårdsgata 112, 5008 Bergen, Norway
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1 citations as recorded by crossref.
Discussed (final revised paper)
Latest update: 14 Dec 2024
Short summary
The Faroe Bank Channel is one of the main passages for the flow of cold dense water from the Arctic into the depths of the world ocean where it feeds the deep branch of the AMOC. Based on in situ measurements, we show that the volume transport of this flow has been stable from 1995 to 2015. The water has warmed, but salinity increase has maintained its high density. Thus, this branch of the AMOC did not weaken during the last 2 decades, but increased its heat transport into the deep ocean.
The Faroe Bank Channel is one of the main passages for the flow of cold dense water from the...