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Thermohaline Circulation, Rob Snyder
Thermohaline Circulation, Rob Snyder
IPY STEM Polar Connections
Surface currents, such as the Gulf Stream, are pushed by the wind. Deep ocean currents, called the “Thermohaline Circulation”, are the result of changes in the density of water. In this activity you can investigate how differences in the temperature and salinity of water can produce deep ocean currents