Linked from

The 46 pages that link to Thermohaline circulation, each with the reason it gives.

• PleistoceneRelated: Changes in this circulation amplified climate shifts during the last glacial period.

• Atlantic OceanNarrower topic: This broader circulation framework explains the density-driven deep flow within the Atlantic.

• Pacific OceanRelated: Deep water formation connects the Pacific to the wider ocean system.

• Atlantic meridional overturning circulationRelated: Density contrasts help drive deep-water formation, though winds also shape the overturning.

• SalinityRelated: Salinity contributes to the density contrasts that help drive deep-ocean circulation.

• Antarctic Circumpolar CurrentCompared with: Density forcing distinguishes this broad circulation mechanism from the current’s strong wind-driven flow.

• Ocean circulationBroader topic: Density contrasts help form and move deep water masses.

• North SeaRelated: Density-driven exchange helps renew North Sea waters with Atlantic and northern waters.

• Red SeaRelated: Dense, salty water formed in the Red Sea sinks and exits through the southern strait.

• UpwellingCompared with: It describes basin-scale density circulation rather than the localized rise of deep water.

• ClimateRelated: Deep-ocean transport moves heat and carbon and affects climate over long timescales.

• OligoceneRelated: Changes in ocean circulation redistributed heat as continents and seaways shifted.

• Tidal currentCompared with: Its slow density-driven circulation contrasts with locally reversing tidal flow.

• Ocean currentRelated: Connects density contrasts to deep currents that transport water between ocean basins.

• Ekman transportCompared with: It is driven by density differences rather than directly by wind stress.

• Ocean gyreCompared with: It is driven by density contrasts, unlike the primarily wind-driven surface gyres.

• OceanographyRelated: Links surface waters and the deep ocean through density-driven flow.

• Gulf StreamRelated: Density-driven flow connects the Gulf Stream region to deeper parts of Atlantic circulation.

• Ocean stratificationRelated: Stratification affects where dense waters form and how readily they sink and circulate.

• Antarctic Bottom WaterNarrower topic: Antarctic Bottom Water is a deep branch of this density-driven circulation.

• Ocean heat transportRelated: Density-driven currents transport heat through the deep ocean and connect ocean basins.

• Climate modelingRelated: Its slow transport of heat and carbon shapes simulated regional and long-term climate.

• Deep seaRelated: It carries cold deep water across ocean basins and connects distant deep-sea habitats.

• Gulf of MexicoNarrower topic: The gulf’s exchanges with the Atlantic contribute to wider ocean circulation.

• Ice ageRelated: Changes in ocean heat transport can shift regional climate during glacial transitions.

• Last Glacial PeriodRelated: Changes in Atlantic circulation redistributed heat during abrupt climate swings.

• SeawaterBroader topic: It links seawater’s temperature and salt content to deep-ocean movement.

• North Atlantic CurrentRelated: Density changes help connect the current’s surface waters to sinking and return flows farther north.

• Glacial periodRelated: Changes in ocean heat and carbon transport affect the pace and pattern of glacial climate.

• Ocean anoxiaRelated: It transports oxygen into the deep ocean and controls how quickly depleted waters are renewed.

• Seawater densityRelated: Density contrasts help sink and transport water masses through the global ocean.

• HydrosphereRelated: It transports heat through the ocean and influences regional climates.

• Philippine SeaNarrower topic: Dense water formed in the sea contributes to circulation between the Pacific’s depths and surface.

• Antarctic ConvergenceRelated: Density contrasts across the boundary contribute to exchanges between water masses.

• South Pacific OceanNarrower topic: It links South Pacific waters to deep and global ocean circulation.

• Arctic Ocean circulationNarrower topic: It supplies the density-driven framework behind deep and intermediate Arctic water movement.

• OceanBroader topic: It describes deep-water movement shaped by ocean temperature and salt content.

• Physical oceanographyBroader topic: It describes how density contrasts drive deep and basin-scale flows.

• SkagerrakNarrower topic: Temperature and salinity differences help drive the strait’s water exchange.

• Alaska pollockNarrower topic: Ocean circulation helps shape the North Pacific conditions that sustain pollock habitat.

• Levantine SeaNarrower topic: Density differences help drive water movement through the eastern Mediterranean.

• Body of waterRelated: It transports heat and dissolved substances through the connected oceans.

• Marine chemistryRelated: It transports dissolved substances across basins and between ocean depths.

• Ocean dynamicsBroader topic: Density contrasts help drive deep currents beyond the reach of direct wind forcing.

• Polar regionsRelated: Polar cooling and sea-ice formation help create dense waters that drive deep-ocean flows.

• Properties of waterRelated: Water density changes help power deep-ocean transport of heat and dissolved material.