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SAN FRANCISCO, Jan. 16 (Xinhua) -- A new research shows the fierce winds circling Antarctica, an important lever on the global climate, shifted quickly in response to the Northern Hemisphere temperature spikes during the last ice age, tens of thousands of years ago.
The findings, published in the January issue of Nature Geoscience, were based on evidence from a West Antarctic ice core 2 miles, or 3.2 kilometers, in length. The ice core's thick annual layers provide precise dating that allows researchers to match its climate history with those in distant Greenland ice records.
During the last ice age, as part of a dramatic pattern in our planet's climate history, which involves paroxysms in Arctic temperatures, Greenland repeatedly warmed by about 10 degrees Celsius over just a few decades and then gradually cooled, while the Southern Hemisphere climate stayed fairly stable, with only weak and long-delayed echoes of the temperature chaos up north.
The wild northern temperature swings, known as Dansgaard-Oeschger events, are thought to be natural oscillations in the climate system.
The Antarctic ice core shows that Southern Ocean winds shifted at the same time, or at most within a few decades, of each rapid Greenland warming event. Antarctic air temperatures, on the other hand, are connected through the slower-moving oceans and took about two centuries to respond.