Articles | Volume 14, issue 2
https://doi.org/10.5194/os-14-259-2018
https://doi.org/10.5194/os-14-259-2018
Research article
 | 
03 Apr 2018
Research article |  | 03 Apr 2018

Estimation of oceanic subsurface mixing under a severe cyclonic storm using a coupled atmosphere–ocean–wave model

Kumar Ravi Prakash, Tanuja Nigam, and Vimlesh Pant

Viewed

Total article views: 3,359 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,127 1,131 101 3,359 78 88
  • HTML: 2,127
  • PDF: 1,131
  • XML: 101
  • Total: 3,359
  • BibTeX: 78
  • EndNote: 88
Views and downloads (calculated since 10 Oct 2017)
Cumulative views and downloads (calculated since 10 Oct 2017)

Viewed (geographical distribution)

Total article views: 3,359 (including HTML, PDF, and XML) Thereof 3,070 with geography defined and 289 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 22 Nov 2024
Download
Short summary
Parameters at the sea surface are determined by the air–sea fluxes of heat, salt, and momentum. Surface wind speed drives the oceanic surface circulation and mixing of temperature and salinity up to a certain depth (mixed layer depth) from the sea surface. In this study, we examined the oceanic mixing process using numerical models under strong cyclonic winds. Results highlight the important role of inertial oscillations in subsurface mixing.