Articles | Volume 12, issue 2
https://doi.org/10.5194/os-12-533-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/os-12-533-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Seasonal hydrography and surface outflow in a fjord with a deep sill: the Reloncaví fjord, Chile
Facultad de Ciencias del Mar y de Recursos Naturales, Universidad de Valparaíso, Viña del Mar, Chile
Center for Oceanographic Research in the Eastern South Pacific (COPAS)-Sur Austral, Universidad de Concepción, Concepción, Chile
Ursula Cifuentes
Center for Oceanographic Research in the Eastern South Pacific (COPAS)-Sur Austral, Universidad de Concepción, Concepción, Chile
Departamento de Oceanografía y Medio Ambiente, Instituto de Fomento Pesquero, Valparaíso, Chile
Oscar Pizarro
Center for Oceanographic Research in the Eastern South Pacific (COPAS)-Sur Austral, Universidad de Concepción, Concepción, Chile
Departamento de Geofísica, Universidad de Concepción, Concepción, Chile
Instituto Milenio de Oceanografía, Universidad de Concepción, Concepción, Chile
Leif Djurfeldt
Department of Oceanography, Earth Sciences Center, Gothenburg University, Gothenburg, Sweden
Mario Caceres
Facultad de Ciencias del Mar y de Recursos Naturales, Universidad de Valparaíso, Viña del Mar, Chile
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Saved (preprint)
Latest update: 23 Nov 2024
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.
The upper layer of the Reloncaví fjord, Chile, shows a continuous stratification year-round....