Abstract:The behaviours of density current were visualised in a simple cylindrical tank and a hydraulic model shaped as Ariake Bay, set in a rotating tank. In both, water was stratified by dissolving salt in the lower layer. In the cylindrical tank, the spread of density current was well parameterised by newly proposed dimensionless numbers. When the Rossby number decreases, we observed that the current was divided into two parts. This may be interpreted as baroclinic instability. In Japan, recently, there is a big dis… Show more
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