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The global conveyor belt moves much more slowly than surface currents -- a few centimeters per second, compared to tens or hundreds of centimeters per second. Scientists estimate that it takes one section of the belt 1,000 years to complete one full circuit of the globe.
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The ocean slowly turns over from top to bottom in a continual global loop. Like a conveyor belt, thermohaline circulation moves nutrients from one part of the ocean to another. Let's start in the northern Atlantic Ocean and follow the conveyor belt as it moves water around the planet. In the seas near Greenland and Norway, the water is cold.
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A global "conveyor belt" is set in motion when deep water forms in the North Atlantic, sinks, moves south, circulates around Antarctica, and then moves northward to the Indian, Pacific, and Atlantic basins. A simplified version of the global conveyor belt is shown in Figure 1, below.
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A process known as thermohaline circulation, or the ocean conveyor belt, drives these deep, ... Scientists realized the ocean was slowly turning over from top to bottom in a continuous global loop. Like a conveyor belt, thermohaline circulation moves nutrients from one part of the ocean to another.
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In the Atlantic Ocean, a giant 'conveyor belt' carries warm waters from the tropics into the North Atlantic, where they cool and sink and then return southwards in the deep ocean. This circulation pattern is an important player in the global climate, regulating weather patterns in the Arctic, Europe, and around the world.
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The global conveyor belt is a system of ocean currents that transport water around the world. While wind primarily propels surface currents, deep currents are driven by differences in water densities in a process called thermohaline circulation. Density depends on both the
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