The following two statements describe forces that move water within the global ocean conveyor belt:
- Water freezes, causing the saltier and denser remaining liquid water to sink.
- Wind pushes surface water away from shore, and cold water rises to replace it.
What is global ocean conveyor belt?
- The ocean conveyor begins in the Norwegian Sea, where warm Gulf Stream water warms the atmosphere in the freezing northern latitudes.
- This heat loss to the atmosphere cools and densifies the water, causing it to sink to the ocean's bottom.
- The cooler water dips and travels south to create place for the incoming warm water as more warm water is brought north.
- This frigid bottom water travels all the way down to Antarctica south of the equator.
- The cold bottom waters eventually rise to the top due to mixing and wind-driven upwelling, extending the global conveyor belt.
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