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Surface waters freeze as they arrive at the cold waters of the North Atlantic. The freezing syste eliminates water particles, yet not salt, from the

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Surface waters freeze as they arrive at the cold waters of the North Atlantic. The freezing syste eliminates water particles, yet not salt, from the sea. The outcome is an expansion in the salti waters. With expanded saltiness and diminished temperature comes more prominent thickne is densest at 4'C - and the water sinks to the sea floor. This cycle sets up an enormous, slow, water "transport line" that transports water along the sea depths to Antarctica then through t Pacific, and ultimately Atlantic seas

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