Articles | Volume 12, issue 2
https://doi.org/10.5194/os-12-533-2016
https://doi.org/10.5194/os-12-533-2016
Research article
 | 
12 Apr 2016
Research article |  | 12 Apr 2016

Seasonal hydrography and surface outflow in a fjord with a deep sill: the Reloncaví fjord, Chile

Manuel I. Castillo, Ursula Cifuentes, Oscar Pizarro, Leif Djurfeldt, and Mario Caceres

Viewed

Total article views: 4,004 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,076 1,714 214 4,004 181 227
  • HTML: 2,076
  • PDF: 1,714
  • XML: 214
  • Total: 4,004
  • BibTeX: 181
  • EndNote: 227
Views and downloads (calculated since 29 Oct 2015)
Cumulative views and downloads (calculated since 29 Oct 2015)
Latest update: 07 Feb 2026
Download
Short summary
The upper layer of the Reloncaví fjord, Chile, shows a continuous stratification year-round. Nevertheless, the vertical salt flux seems to be balanced by the horizontal salt flux, which maintains the amount of salt into the fjord nearly as a steady state. The upper layer shows a flushing time of about 3 days.
Share