Surface currents and thermohaline flow
The ocean's deep water currents are driven by gravity and coriolis force. Stratification in the deep ocean caused by different water masses leads to density layers that sink or rise to achieve neutral buoyancy. In turn, density is controlled by salinity and temperature characteristics.
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Author: Sean Todd Email: stodd@coa.edu Home Page: http://www.coa.edu/faculty/webpages/stodd/index. Other information: Download presentation source |