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- Deep currents, also known as thermohaline circulation, result from differences in water density1. They are characterized by2:
- Extremely cold water temperatures
- Relatively high concentration of oxygen
- High salt levels
- Very dense water
Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.Deep currents, also known as thermohaline circulation, result from differences in water density. These currents occur when cold, dense water at the poles sinks. Surface water flows to replace sinking water, causing a conveyor belt-like effect of water circulating around the globe on a 1000-year journey.www.sofarocean.com/posts/understanding-surface …Deep currents can be distinguished by the extremely cold water temperatures, the relatively high concentration of oxygen and the high salt levels that all result from sinking surface water. Because of these conditions, the water in deep ocean currents is also very dense.sciencing.com/deep-currents-8118821.htmlPrevailing winds, ocean-surface currents, and the associated mixing influence the physical, chemical, and biological characteristics of the ocean, as well as global climate. Deep ocean currents are density -driven and differ from surface currents in scale, speed, and energy.www.nationalgeographic.org/media/ocean-current…- Deep ocean current circulation begins in the North Atlantic where cold, dense, salty water sinks and flows southward at great depths.
- Next it moves into the South Atlantic.
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WEBJan 11, 2021 — Deep Currents. Currents also flow deep below the surface of the ocean. Deep currents are caused by differences in density at the top and bottom. More dense water takes up less space than less dense …
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WEBDeep Currents. Surface currents occur close to the surface of the ocean and mostly affect the photic zone. Deep within the ocean, equally important currents exist that are called deep currents. These currents are not …
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WEBFeb 24, 2012 — Cold water (blue lines) sinks in the North Atlantic, flows along the bottom of the ocean and upwells in the Pacific or Indian. The water then travels in surface currents (red lines) back to the North Atlantic. Deep water also forms off of Antarctica.
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WEBThermohaline circulation drives deep ocean currents. Upwelling of cold, nutrient-rich waters creates biologically rich areas where surface waters are blown away from a …
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WEBHowever, changing the density of the surface water causes it to sink or rise, and these vertical, density-driven movements create the deep ocean currents. These thermohaline currents are slow, on the order of 10-20 km per year compared with surface currents that move at several kilometers per hour. Water masses.
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