Articles | Volume 13, issue 6
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


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Laura Cimoli on behalf of the Authors (11 Jul 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (21 Jul 2017) by John M. Huthnance
ED: Publish subject to technical corrections (04 Aug 2017) by John M. Huthnance
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.