Articles | Volume 12, issue 6
Ocean Sci., 12, 1205–1220, 2016
Ocean Sci., 12, 1205–1220, 2016

Research article 17 Nov 2016

Research article | 17 Nov 2016

A stable Faroe Bank Channel overflow 1995–2015

Bogi Hansen et al.


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Bogi Hansen on behalf of the Authors (11 Oct 2016)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (14 Oct 2016) by Mario Hoppema
RR by Anonymous Referee #2 (27 Oct 2016)
ED: Publish subject to technical corrections (27 Oct 2016) by Mario Hoppema
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.