Articles | Volume 12, issue 6
https://doi.org/10.5194/os-12-1205-2016
https://doi.org/10.5194/os-12-1205-2016
Research article
 | 
17 Nov 2016
Research article |  | 17 Nov 2016

A stable Faroe Bank Channel overflow 1995–2015

Bogi Hansen, Karin Margretha Húsgarð Larsen, Hjálmar Hátún, and Svein Østerhus

Viewed

Total article views: 2,964 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,803 1,013 148 2,964 496 117 131
  • HTML: 1,803
  • PDF: 1,013
  • XML: 148
  • Total: 2,964
  • Supplement: 496
  • BibTeX: 117
  • EndNote: 131
Views and downloads (calculated since 04 Aug 2016)
Cumulative views and downloads (calculated since 04 Aug 2016)

Viewed (geographical distribution)

Total article views: 2,964 (including HTML, PDF, and XML) Thereof 2,697 with geography defined and 267 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 17 Nov 2024
Download
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.