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Halocine / Internal Seiche

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The Halocline is the zone of the ocean in which salinity increases rapidly with depth.

A Seiche is a pendulum-like rocking of water that may be caused by meteorological or seismic forces. In this case it is occurring at the boundary between liquids of different densities.

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Halocline and Internal Seiche Simulation (1) Halocline and Internal Seiche Simulation (2)
Halocline and Internal Seiche Simulation (3) Halocline and Internal Seiche Simulation (4)



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