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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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Ocean current - Wikipedia
Ocean dynamics define and describe the motion of water within the oceans. Ocean temperature and motion fields can be separated into three distinct layers: mixed (surface) layer, upper ocean (above the thermocline), and deep ocean. Ocean currents are measured in units of sverdrup (sv), where 1 sv is equivalent to a volume flow rate of 1,000,000 m (35,000,000 cu ft) per second.
Wikipedia · Text under CC-BY-SA license- Estimated Reading Time: 9 mins
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WEBJan 2, 2024 · Prevailing winds, ocean-surface currents, and the associated mixing influence the physical, chemical, and biological characteristics of the ocean, as well as global …
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WEBAug 1, 2011 · Ocean currents, abiotic features of the environment, are continuous and directed movements of ocean water. These currents are on the ocean’s surface and in its depths, flowing both locally and globally.
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WEBApr 12, 2021 · Deep ocean currents are driven by differences in water density and result from thermohaline circulation. They play a crucial role in regulating the climate and …
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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 …
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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 …
WEBAbstract. The long-standing paradigm for the large-scale time-averaged ocean circulation in the world oceans includes intensified currents at the western boundary, and a much …
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