Thursday, December 09, 2004

Sea-Level Clue to Climate Chill

UIC News Release: "It sounds like a disaster film: rising temperatures melt polar ice, causing a flood of freshwater to rapidly enter the salty North Atlantic. As the fresh and salty water mixes, density changes, altering the Gulf Stream ocean currents that moderate the North Atlantic climate. In just a few years, average temperatures plummet, ushering in a deep freeze that lasts a century or more before fresh and salty water is back in balance, ocean currents adjust and temperatures return to normal. "

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