As warm water from the equator moves towards the poles, it gets colder, and has a higher concentration of salt, because ice crystals that form trap water and leave salt behind. This cold, salty water sinks, and warmer surface water takes its place. This cold, salty water is now at the bottom of the ocean floor, and can only move in one direction: Horizontally. It sometimes rises again near the equator through upwelling, bringing nutrients to the surface. This warm water now moves towards the poles, cools down, gets saltier, and
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