Articles | Volume 22, issue 4
https://doi.org/10.5194/os-22-2333-2026
https://doi.org/10.5194/os-22-2333-2026
Research article
 | 
04 Aug 2026
Research article |  | 04 Aug 2026

Eddy kinetic energy and energy conversion rates along the Atlantic Water boundary current north of Svalbard

Kjersti Kalhagen, Ilker Fer, Till M. Baumann, Jon Albretsen, and Lukas Frank

Viewed

Total article views: 7,274 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
5,285 1,800 189 7,274 235 257
  • HTML: 5,285
  • PDF: 1,800
  • XML: 189
  • Total: 7,274
  • BibTeX: 235
  • EndNote: 257
Views and downloads (calculated since 17 Sep 2025)
Cumulative views and downloads (calculated since 17 Sep 2025)

Viewed (geographical distribution)

Total article views: 7,274 (including HTML, PDF, and XML) Thereof 7,042 with geography defined and 232 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 04 Aug 2026
Download
Short summary
Warm Atlantic Water flowing eastward north of Svalbard loses heat faster than can be explained by cooling to the atmosphere and mixing alone. Using year-long mooring observations and an ocean model, we found that mesoscale variability and energy transfer into eddies are largest in autumn and winter, when the boundary current is also at its strongest and warmest. This mesoscale activity enhances lateral heat exchange and likely contributes to the observed cooling of Atlantic Water along its path.
Share