Ocean Science
Ocean Science
OS
Articles | Volume 20, issue 2
Articles | Volume 20, issue 2
https://doi.org/10.5194/os-20-293-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/os-20-293-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 20, issue 2
Research article
 | 
14 Mar 2024
Research article |  | 14 Mar 2024

Fjord circulation permits a persistent subsurface water mass in a long, deep mid-latitude inlet

Laura Bianucci, Jennifer M. Jackson, Susan E. Allen, Maxim V. Krassovski, Ian J. W. Giesbrecht, and Wendy C. Callendar

Viewed

Total article views: 1,146 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
854 198 94 1,146 79 76
  • HTML: 854
  • PDF: 198
  • XML: 94
  • Total: 1,146
  • BibTeX: 79
  • EndNote: 76
Views and downloads (calculated since 05 Sep 2023)
Cumulative views and downloads (calculated since 05 Sep 2023)

Viewed (geographical distribution)

Total article views: 1,146 (including HTML, PDF, and XML) Thereof 1,107 with geography defined and 39 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Dec 2024
Download
Short summary
While the deeper waters in the coastal ocean show signs of climate-change-induced warming and deoxygenation, some fjords can keep cool and oxygenated waters in the subsurface. We use a model to investigate how these subsurface waters created during winter can linger all summer in Bute Inlet, Canada. We found two main mechanisms that make this fjord retentive: the typical slow subsurface circulation in such a deep, long fjord and the further speed reduction when the cold waters are present.
Read more
Special issue
Oceanography at coastal scales: modelling, coupling, observations,...