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The detailed structure of the thermohaline front at the mouth of Ise Bay during winter has been investigated by intensive field observation. The transport of suspended matter from Ise Bay to the Pacific Ocean through the thermohaline front has also been investigated using the data from a time-series sediment trap, a current meter and a nephelometer moored at the bay mouth station. The mixed coastal and offshore water at the surface of the thermohaline front sinks to a depth of about 200 m in the offshore area.

Variation in the Thermohaline Front at the Mouth of Ise Bay.