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

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Manuel Castillo on behalf of the Authors (09 Mar 2016)  Author's response 
ED: Publish subject to technical corrections (29 Mar 2016) by Oliver Zielinski
AR by Manuel Castillo on behalf of the Authors (31 Mar 2016)  Manuscript 
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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.