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The mechanisms are temperature and circulation.

Sea ice concentrates salt. Seas in the Southern Ocean -- the Weddell and the Ross -- freeze over during the Antarctic winter -- and during that process produce polynyas which open surface water to the cold winds that blow off the continent. This freezes the water more quickly and . . . concentrates the minerals.

The water becomes laden with salt, and is colder, so it sinks, creating Antarctic bottom water.

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Q: What is the mechanisim responsible for causing the very high density of Antarctic bottom water?
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