thermohaline circulation
collocation in Englishmeaningsofcirculation
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circulation
noun
uk/ˌsɜː.kjəˈleɪ.ʃən/us/ˌsɝː.kjəˈleɪ.ʃən/
the process in which something such as information, money, or goods passes from one person ...
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(Definition ofcirculationfrom theCambridge English Dictionary© Cambridge University Press)
Examplesofthermohaline circulation
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This inversethermohalinecirculationallows dispersion of shallow and cool water species in open oceanic environments in the photic zone above the thermocline level.
From theCambridge English Corpus
Our knowledge of thethermohalinecirculationof the oceans is advancing rapidly.
From theCambridge English Corpus
He is also known for his work onthermohalinecirculation.
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Wikipedia
Stommel also developed early models of thethermohalinecirculationwhich suggested that it might have more than one stable state.
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Thethermohalinecirculationis sometimes called the ocean conveyor belt, the great ocean conveyor, or the global conveyor belt.
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Due to the constantthermohalinecirculationfronts, cold air flows near the surface and bottom of the ocean.
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Thermohalinecirculationdetermines the relative ages of the water in these basins.
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Surface heat and freshwater fluxes create global density gradients that drive thethermohalinecirculationpart of large-scale ocean circulation.
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This is the beginning of thethermohalinecirculation.
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Thermohalinecirculationmay be altered by increasing amounts of freshwater in the ocean.
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A major controlling factor in oceanic-atmospheric carbon exchange isthermohalinecirculation.
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Thermohalinecirculationcan bring carbon in the deep ocean levels to the upper levels, where it can again be exchanged with the atmosphere.
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Deep water formation simply means surface water being transported downwards into the ocean, this is important to drive the global ocean currents bythermohalinecirculation.
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This exportation of freshwater helps control thethermohalinecirculationand the global climate.
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A main deep ocean current flows through all the world's oceans and is known as thethermohalinecirculationor global conveyor belt.
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The movement of water due to differences in density as a function of water temperature and salinity is calledthermohalinecirculation.
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The whole ocean is involved in slowthermohalinecirculation.
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Salinity in combination with temperature determine ocean circulation by defining its density and hencethermohalinecirculation.
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Thisthermohalinecirculation, occurs at both deep and shallow ocean levels and moves much slower than tidal or surface currents.
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Ocean currents are also important factors in determining climate, particularly thethermohalinecirculation that distributes thermal energy from the equatorial oceans to the polar regions.
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These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.
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