1994
DOI: 10.1016/0278-4343(94)90089-2
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Spatial variation of the annual cycle of temperature in the Patagonian shelf between 40 and 50° of south latitude

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Cited by 34 publications

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“…During ebb tides seawater is expelled through the mouth to SMG, forming eddies moving northwards for up to 100 km, reaching the center of SMG (Amoroso and Gagliardini, 2010). Considering that the mean tidal amplitude of SJG is 6 m and that the mean depth of the gulf is 40 m, the volume of seawater flowing through the mouth in every rising and ebb tide represents approximately 15% of its total volume (Rivas, 1990). Furthermore, since the process is asymmetrical between domains, this figure must be even higher for the western domain, explaining the homogeneous structure of the water column in it.…”
Section: Discussion
mentioning
confidence: 99%