A thermohaline current is affected by differences in water temperature and salinity. These differences drive the circulation of deep ocean waters around the globe, transporting heat and nutrients to different regions and influencing climate patterns.
Salinity affects thermohaline circulation by influencing the density of seawater. Higher salinity increases water density, promoting sinking of cold, dense water in polar regions. Temperature influences this circulation by controlling the density of water - colder water is denser and more likely to sink. Both factors work together to drive the global thermohaline circulation system.
Thermohaline circulation is a global pattern of ocean currents driven by differences in temperature and salt concentration. It plays a crucial role in distributing heat around the planet and regulating climate. This circulation helps transport nutrients and oxygen throughout the ocean, influencing marine ecosystems.
The thermohaline circulation is important because it helps distribute heat and nutrients around the globe, influencing climate patterns and marine ecosystems. It plays a crucial role in regulating Earth's climate by transporting warm water towards the poles and cold water towards the equator. Any disruption to this circulation pattern can have far-reaching impacts on weather patterns and ecosystems worldwide.
The name of the strongest and fastest ocean current in the world is the Agulhas Current.
Another name for thermohaline current is "conveyor belt," which some call this current of the ocean.
Global Ocean Conveyor
Another name for thermohaline circulation is the ocean conveyor belt. This circulation pattern involves the movement of water around the world's oceans based on differences in temperature and salinity.
The Great Ocean Conveyor Belt is also called thermohaline circulation.
A thermohaline current is affected by differences in water temperature and salinity. These differences drive the circulation of deep ocean waters around the globe, transporting heat and nutrients to different regions and influencing climate patterns.
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thermohaline circulation
By the mixtures temperatures rising and lowering and salinity(amount of salt in sea water)
The two characteristics of water that combine to form a thermohaline current are temperature and salinity. As water becomes cold and more saline, it becomes denser and sinks to the ocean floor, driving the vertical circulation of the ocean known as the thermohaline circulation.
"Thermo" in "thermohaline" refers to heat or temperature. "Thermohaline" describes ocean currents driven by differences in temperature and salinity.
A thermohaline current is a gravity current. It is driven by gravity. The root idea is that fluids of different densities are acted on differently by gravity, and gravity "pulls" more on more dense fluids. That means cooler or more salty water, which is more dense than warmer or less salty water, will be "pulled down" more, and will displace the warmer or less salty and "dive deep" to set up deep ocean currents. Use the links below to learn more.
The "north Atlantic current" is very strong.I really like the "north Atlantic current."The "north Atlantic current" is driven by the global thermohaline circulation (THC), it is wind driven