Abstract
Data obtained using a temperature-salinity-depth recorder in the Tasman Sea in
1965 show salinity anomalies at depths between 200 and 800 m. It is suggested that
these are produced by an outflow of saline water from Bass Strait.
Subject
Ecology,Aquatic Science,Ecology, Evolution, Behavior and Systematics,Oceanography
Cited by
12 articles.
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