Articles | Volume 11, issue 3
https://doi.org/10.5194/os-11-343-2015
https://doi.org/10.5194/os-11-343-2015
Research article
 | 
12 May 2015
Research article |  | 12 May 2015

Deep drivers of mesoscale circulation in the central Rockall Trough

T. J. Sherwin, D. Aleynik, E. Dumont, and M. E. Inall

Viewed

Total article views: 3,116 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,762 1,168 186 3,116 379 159 170
  • HTML: 1,762
  • PDF: 1,168
  • XML: 186
  • Total: 3,116
  • Supplement: 379
  • BibTeX: 159
  • EndNote: 170
Views and downloads (calculated since 25 Nov 2014)
Cumulative views and downloads (calculated since 25 Nov 2014)

Cited

Saved (final revised paper)

Saved (preprint)

Latest update: 21 Nov 2024
Download
Short summary
The Rockall Trough feeds warm salty water to Polar regions and the European Shelf. Detailed observations from an underwater glider show that a) the meandering surface current field in the central trough is driven by deep eddies; b) chance circulations deflect the eastern slope current and warm the western side; c) and altimeter observations omit the mean flow in the narrow slope current. There are wider implications for satellite altimeter observations, ocean monitoring and ocean model results.