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Circulation in Marginal Seas and Estuaries

Circulation in Marginal Seas and Estuaries

Thermohaline circulation can drive water flow in marginal seas. Circulation and stratification in estuaries is determined by the mixing of less dense river water and denser ocean water.

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Exploring Our Fluid Earth, a product of the Curriculum Research & Development Group (CRDG), College of Education. University of Hawaii, 2011. This document may be freely reproduced and distributed for non-profit educational purposes.