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Seasonal data on temperature, salinity, dissolved oxygen (DO) andchlorophyll, combined with meteorological and river discharge time series,were used to describe the oceanographic conditions of the Reloncaví fjord(41°35′ S, 72°20′ W). The winds in the fjord valleymainly blow down-fjord during the winter, reinforcing the upper layeroutflow, whereas the winds blow predominantly up-fjord during the spring andsummer, contrary to the upper layer outflow. The fjord, with a deep sill atthe mouth, was well stratified year-round and featured a thin surface layerof brackish water with mean salinities between 10.4 ± 1.4 (spring) and13.2 ± 2.5 (autumn). The depth of the upper layer changed slightlyamong the different studied seasons but remained at 4.5 m near the mouth.This upper layer presented a mean outflow (Q1) of 3185 ± 223 m3 s−1, which implies a flushing time of 3 days for this layer. The vertical salt flux was  ∼  37 tons of salt per second, similar to the horizontal salt flux observed in the upper layer. These estimates will contribute to better management of the aquaculture in this region

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