Antarctic Iceberg Flotilla Caused Huge Sea-Level Rise: Page 2


Drilling for clues

To find out how the ice sheet fared under natural warming conditions, researchers drilled deep into the Scotia seafloor between Antarctica and South America. They discovered sandy debris from eight iceberg surges in the past 20,000 years. Icebergs carry sand trapped in ice out to sea, and the sediment falls onto the ocean floor as the frozen chunks melt.

The biggest pulse of debris was 14,600 years ago, at the same time as a global sea-level rise of about 13 feet (4 m) within 100 years, said study co-author Axel Timmermann, a climate scientist at the University of Hawaii at Manoa. Because ice sheets in the Northern Hemisphere were melting at the same time, scientists think Antarctica's melting accounts for about half of this jump in sea level, he said.

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When glaciers draw back, they drop icebergs that melt and raise sea level. Ice melting from contact with warmer seawater can also contribute to sea-level rise.

During this period of rapid sea-level rise, dubbed meltwater pulse 1A, sea level rose 20 times faster than today's rate. Between 14,650 and 14,310 years, the oceans encroached on land by an astonishing 46 to 59 feet (14 to 18 m), or 13 feet (4 m) per century.

"The question has been, 'Where did this ice come from?'" Clark told Live Science. "This is the first clear evidence Antarctica did contribute to this sea-level rise."

The findings suggest that Antarctica's giant glaciers respond to a warming climate with pulses of quick withdrawal, rather than a slow and steady retreat. But the discovery does not answer one of Antarctica's biggest mysteries — what triggered the melting, and why did the glaciers stop their galloping retreat. Nor do researchers know which parts of the ice sheet were responsible for the icebergs, though they suspect it was primarily the Antarctic Peninsula and the Weddell Sea region.

Modeling suggests that the massive melting causes ocean circulation changes that prompt a feedback loop, letting warmer ocean water reach the ice, Timmermann said. "There is a positive feedback that can happen," he said.

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