The ocean is not a still body of water. There is constant motion in the ocean in the form of a global ocean conveyor belt. This motion is caused by a combination of thermohaline currents thermo temperature haline salinity in the deep ocean and winddriven currents on the surface.
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they are factors that affect the direction and speed of surface and deep water ocean currents. what is the global conveyor belt why is it called a 34conveyor belt34 a large system of thermohailine circulation. it is called this because its circulation of warm and cold water acts as an underwater 39river39 that moves water throughout the entire ocean
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I can explain the causes for surface ocean currents. Surface currents are mainly caused by winds, solar heating, and the Coriolis effect I can explain the driving force for deep ocean currents global conveyor belt Differences in the density of deep ocean water. The movement of cold water upward from the deep ocean.
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The global conveyer belt is part of the largescale ocean circulation that is driven by differences in the density of the waters. It plays a key role in keeping the climate at balance and Europe
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The ocean circulation conveyor belt helps balance climate. As part of the ocean conveyor belt, warm water from the tropical Atlantic moves poleward near the surface where it gives up some of its heat to the atmosphere. This process partially moderates the cold temperatures at higher latitudes.
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The global conveyor belt carries water and heat energy across the globe. What is the difference in how the conveyor belt moves water in the tropics compared to the tropic Water warms and becomes less dense, so it rises toward the surface.
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Cold water has a higher density than warm water. Water gets colder with depth because cold, salty ocean water sinks to the bottom of the ocean basins below the less dense warmer water near the surface. The sinking and transport of cold, salty water at depth combined with the winddriven flow of warm water at the surface creates a complex pattern of ocean circulation called the 39global conveyor
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Thermohaline Circulation. evaporationsea ice formation cause water to move. Wind Driven Currents. Once in motion, an ocean current can be slowed by friction, deflected by the Coriolis effect, blocked by coastlines continents, islands, etc, or altered by horizontal pressure gradients. Transfered by the Ocean Conveyor Belt Trapped
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The sinking of cold water creates a current that 34sucks in34 warm water from the equator to replace the sinking water, setting the whole global conveyor belt in motion. The main driver of the ocean conveyor belt is the unequal heating of the ocean water by the sun more at the equator, less at the poles and the difference of water densities
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The Global Conveyor Belt is dependent on thermohaline circulation. When less North Atlantic Deep Water forms, less CO2g is absorbed from the atmosphere into the ocean. As more CO2g is let into the atmosphere through less North Atlantic Deep Water currents forming, Earths global temperature increases because of the greenhouse effect.
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This deepwater current is known as the global conveyor belt and is driven by density differences in the water. Water movements driven by differences in density are also known as thermohaline circulation because water density depends on its temperature thermo and salinity haline.
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The ocean is not a still body of water. There is constant motion in the ocean in the form of a global ocean conveyor belt. This motion is caused by a combination of thermohaline currents thermo temperature haline salinity in the deep ocean and winddriven currents on the surface.
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The great ocean conveyor moves water around the globe. There is constant motion in the ocean in the form of a global ocean conveyor belt. This motion is caused by a combination of thermohaline currents thermo temperature haline salinity in the deep ocean and winddriven currents on the surface.
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The David Suzuki Foundation describes the basics of the Great Ocean Conveyor Belt and explains the potential effects global warming could have. Great Ocean Conveyor Belt The United Nations Environment Programme presents a helpful world map illustrating the threedimensional movement of the thermohaline circulation.
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Winds drive ocean currents in the upper 100 meters of the oceans surface. However, ocean currents also flow thousands of meters below the surface. These deepocean currents are driven by differences in the waters density, which is controlled by temperature thermo and salinity haline. This process is known as thermohaline circulation.
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Thermohaline circulation THC is a part of the largescale ocean circulation that is driven by global density gradients created by surface heat and freshwater fluxes. The adjective thermohaline derives from thermoreferring to temperature and haline referring to salt content, factors which together determine the density of sea water.
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The global conveyor belt is a strong, but easily disrupted process. Research suggests that the conveyor belt may be affected by climate change. If global warming results in increased rainfall in the North Atlantic, and the melting of glaciers and sea ice, the influx of warm freshwater onto the sea surface could block the formation of sea ice, disrupting the sinking of cold, salty water.
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Thermohaline circulation drives a globalscale system of currents called the global conveyor belt. The conveyor belt begins on the surface of the ocean near the pole in the North Atlantic. Here, the water is chilled by arctic temperatures. It also gets saltier because when sea ice forms, the salt does not freeze and is left behind in the
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The Global Conveyor Belt As previously mentioned, the global conveyor belt describes the current that runs throughout the earths waters, driven by the cold waters at the poles. The belt starts in the North Atlantic Ocean, where cold water that surrounds the ice sinksthe , and starts to flow around the world.
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explain what causes the movement of water in the global conveyorbelt circulation it is associated with thermohaline circulation, in which cold, dense, relatively salty ocean water sinks in highlatitude ocean areas this cold, dense water slowly flows along the bottom of the ocean, eventually to rise into warmer, shallow currents
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The global conveyor belt includes both surface and deep ocean currents that circulate the globe in a 1,000year cycle. The global conveyor belts circulation is the result of two simultaneous processes warm surface currents carrying less dense water away from the Equator toward the poles, and cold deep ocean currents carrying denser water
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The global conveyor belt carries water and heat energy across the globe. What is the difference in how the conveyor belt moves water in the tropics compared to the tropic? Water warms and becomes less dense, so it rises toward the surface.
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