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Listen to native speakers pronounce “ocean bottom” in real conversational contexts with synchronized timestamps and subtitles.
Oceans pump tons of water around the world in a so-called “global conveyor belt” of currents, mostly driven by changes in temperature and saltiness.Basically, water that's saltier and colder is more dense and sinks, traveling along the deep ocean bottom.While water that's less salty and warmer is less dense and upwells.
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