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Heat Release from Stagnant Deep Sea Helped End Last Ice Age

The build-up and subsequent release of warm, stagnant water from the deep Arctic Ocean and Nordic Seas played a role in ending the last Ice Age within the Arctic region, according to new research led by an international team of scientists.

The study, published today in Science, examines how the circulation of the combined Arctic Ocean and Nordic Seas – called the Arctic Mediterranean – changed since the end of the last Ice Age (~20,000-30,000 years ago). The results highlight the important impact that changes in ocean circulation can have on climate.

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WHOI Scientist to Receive American Meteorological Society Award

A physical oceanographer known for his theories of wind driven ocean circulation and the fluid dynamics of the oceans will receive the 2005 Sverdrup Gold Medal from the American Meteorological Society (AMS), the nation’s leading professional society for scientists in the atmospheric and related sciences, in ceremonies January 12 at the AMS annual meeting in San Diego.

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