The term thermohaline circulation ( THC ) refers to the part of the large-scale ocean circulation that is driven by global density gradients created by surface heat and freshwater fluxes
Thermohaline circulation is also called overturning circulation. It is driven by density. The time scale for thermohaine is 1000 years.
The Great Ocean Conveyor Belt is also called thermohaline circulation.
Thermohaline currents, also known as ocean circulation currents, are caused by temperature and salinity differences in the water. These currents play a crucial role in distributing heat around the globe and influence climate patterns.
The sun heats the water, causing cold / hot circulation, and evaporation. It also heats the air, causing wind, which also moves currents.
Temperature differences in water
Surface currents are ocean currents that occur near the surface of the ocean and are driven by factors like wind, the Earth's rotation, and surface water density. Deep currents, also known as thermohaline currents, are ocean currents that flow deep beneath the surface and are driven by differences in water temperature and salinity. They are much slower and can extend thousands of meters below the surface.
The Atlantic thermohaline circulation, also known as the Atlantic Meridional Overturning Circulation (AMOC), is a large system of ocean currents that transport warm, salty water northward in the Atlantic Ocean and colder, fresher water southward. It plays a crucial role in regulating Earth's climate by distributing heat around the globe. Disruption of the AMOC can have significant impacts on regional and global climate patterns.
The global ocean conveyor belt, also known as the thermohaline circulation, is a system of deep-ocean circulation driven by density differences caused by variations in temperature and salinity. It plays a crucial role in distributing heat around the Earth and regulating climate. Warm surface currents move towards the poles, where they cool, become denser, and sink, forming deep ocean currents that then circulate back towards the equator.
The thermohaline circulation is a term for the global density-driven circulation of the oceans. Derivation is from thermo- for heat and -haline for salt, which together determine the density of sea water
becuase the ocean is a part of the renable energy surces
As the equator is warm, the currents that originate from there are also warm.