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Ars Technica
Mar 27, 2015, 4:20 pm134 ptsIf ocean circulation has an Achilles’ heel, it’s the North Atlantic. Here, salty surface water from the south cools, becoming dense enough to mix with the deep water below. Once in the deep, it turns to make a return journey southward. This mixing is a delicate balance—dump enough lower-salinity water at…
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