Nasa The Thermohaline Circulation The Great Ocean Conveyor Be This usually occurs in the equatorial ocean, mostly in the pacific and indian oceans. this very large, slow current is called the thermohaline circulation because it is caused by temperature and salinity (haline) variations. this animation shows one of the major regions where this pumping occurs, the north atlantic ocean around greenland. The thermohaline circulation the great ocean conveyor belt. the oceans are mostly composed of warm salty water near the surface over cold, less salty water in the ocean depths. these two regions don't mix except in certain special areas. the ocean currents, the movement of the ocean in the surface layer, are driven mostly by the wind.
Nasa The Thermohaline Circulation The Great Ocean Conveyor Be The oceans are mostly composed of warm salty water near the surface over cold, less salty water in the ocean depths. these two regions don't mix except in ce. Nasa goddard space flight center scientific visualization studio. this nasa animation depicts thermohaline circulation in the ocean and how it relates to salinity and water density. it illustrates the sinking of water in the cold, dense ocean near iceland and greenland. the surface of the ocean then fades away and the animation pulls back to. The thermohaline circulation, often referred to as the ocean's "conveyor belt", links major surface and deep water currents in the atlantic, indian, pacific, and southern oceans. multiple mechanisms conspire to increase the density of surface waters at high latitudes. cold winds blowing over the oceans chill the waters beneath them. This nasa animation depicts thermohaline circulation in the ocean and how it relates to salinity and water density. it illustrates the sinking of water in the cold, dense ocean near iceland and greenland. the surface of the ocean then fades away and the animation pulls back to show the global thermohaline circulation system.
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