Ocean Science
Ocean Science
OS
Articles | Volume 19, issue 6
Articles | Volume 19, issue 6
https://doi.org/10.5194/os-19-1669-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-19-1669-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 19, issue 6
Research article
 | Highlight paper
 | 
30 Nov 2023
Research article | Highlight paper |  | 30 Nov 2023

Constraining an eddy energy dissipation rate due to relative wind stress for use in energy budget-based eddy parameterisations

Thomas Wilder, Xiaoming Zhai, David Munday, and Manoj Joshi

Viewed

Total article views: 1,696 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,460 179 57 1,696 47 45
  • HTML: 1,460
  • PDF: 179
  • XML: 57
  • Total: 1,696
  • BibTeX: 47
  • EndNote: 45
Views and downloads (calculated since 28 Jun 2023)
Cumulative views and downloads (calculated since 28 Jun 2023)

Viewed (geographical distribution)

Total article views: 1,696 (including HTML, PDF, and XML) Thereof 1,661 with geography defined and 35 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Dec 2024
Download
Co-editor-in-chief
This analytical study investigates the eddy energy dissipation rate for relative wind stress. The derived dissipation rate draws on our fundamental understanding of relative wind stress damping, vertical eddy structure, and eddy energy. The study suggests a method to parameterise the damping of total eddy energy in coarse resolution global climate models, and may have implications for a wide range of climate processes.
Read more
Short summary
The dissipation rate of eddy energy in current energy budget-based eddy parameterisations is still relatively unconstrained, leading to uncertainties in ocean transport and ocean heat uptake. Here, we derive a dissipation rate due to the interaction of surface winds and eddy currents, a process known to significantly damp ocean eddies. The dissipation rate is quantified using seasonal climatology and displays wide spatial variability, with some of the largest values found in the Southern Ocean.
Read more