Articles | Volume 13, issue 6
https://doi.org/10.5194/os-13-905-2017
https://doi.org/10.5194/os-13-905-2017
Research article
 | 
14 Nov 2017
Research article |  | 14 Nov 2017

Meanders and eddy formation by a buoyant coastal current flowing over a sloping topography

Laura Cimoli, Alexandre Stegner, and Guillaume Roullet

Viewed

Total article views: 2,739 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,455 1,135 149 2,739 123 128
  • HTML: 1,455
  • PDF: 1,135
  • XML: 149
  • Total: 2,739
  • BibTeX: 123
  • EndNote: 128
Views and downloads (calculated since 18 Apr 2017)
Cumulative views and downloads (calculated since 18 Apr 2017)

Viewed (geographical distribution)

Total article views: 2,739 (including HTML, PDF, and XML) Thereof 2,580 with geography defined and 159 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 14 Dec 2024
Download
Short summary
The dispersion of coastal waters offshore strongly depends on the dynamical regime of the current that characterizes the local coastal circulation. By using an idealized model configuration, we identify some key parameters – which can be calculated from observations – that describe when a coastal current flowing over a sloping topography acts as a source of meanders or eddies or as a dynamical barrier to the cross-shore transport.