Linked from

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

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

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

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

• 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.