Transverse variability of flow and density in a Chilean fjord

Measurements of velocity and density profiles were made to describe the transverse structure of the flow in Aysen Fjord, Southern Chile (45.2degreesS and 73.3degreesW). Current profiles were made with a 307.2 kHz acoustic doppler current profiler (ADCP) during 20 repetitions of a cross-Fjord transect during one semidiurnal tidal cycle. The transect had a similar to 320degrees orientation, 3 km length, and its bathymetry consisted of two channels, one on the southern side (230 m depth) and the other on the northern side (180 m depth), separated by a bank ca, 65 m depth, which was located similar to 1 km from the northern coast. Density measurements to a maximum depth of 50 m were made at the extremes of each transect repetition and over the bank. Also, a total of nine CTD stations that covered the surroundings of the bank was sampled 2 days prior to the ADCP sampling. During the sampling period the mean Row showed a three layer structure that was consistent with up-fjord wind-induced exchange: a thin (< 8 m) weak outflow close to the surface due to river discharge; a layer of inflow, (down-wind) underneath attributed to the effect of wind-stress; and a deep compensatory outflow due to the barotropic pressure gradient set up by the wind. The bank caused the strongest wind-induced not inflows and outflows to be shifted to the channels and also disrupted the three-layer structure. Also, the strongest tidal current amplitudes were located over the bank. The near-surface flow and density distributions suggested that the transverse dynamics were ageostrophic in a layer above similar to 50 m. This was indicated by the wind-induced shifting of the location of salt water intrusion from the northern side to the southern side of the Ford. Density measurements also suggested an alternation to quasigeostrophic conditions in this upper layer during calm winds. Below this layer the dynamics remained quasi geostrophic. (C) 2002 Elsevier Science Ltd. All rights reserved.