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You can see temperature decreases with increasing depth. The distribution and formative processes of latent heat polynyas in East Antarctica. Now robots have been developed to search the seas for the dangerous

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Ocean water differs in temperature and salinity. Another use could be to replace expensive desalination plants. DOW is typically used to describe ocean water at sub-thermal depths sufficient to provide a measurable difference in water temperature.

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This is due to a difference in heat capacity. This northward movement amounts to 2. The other part recirculates and some of it flows through the Romanche Fracture Zone into the eastern Atlantic.