http://researchnews.osu.edu/archive/greenmelt.htm {This news release accompanies the press conference, "Greenland Glaciers: What Lies Beneath," to be given Wednesday, December 16, 2009, at 9:00 a.m. PT (12:00 NOON ET) at the American Geophysical Union Meeting in San Francisco (Press conference room, MW 3012).}
GREENLAND GLACIERS: WHAT LIES BENEATH
Researchers learning more about how water beneath glaciers contributes to ice loss
San Francisco -- Scientists who study the melting of Greenland’s glaciers are discovering that water flowing beneath the ice plays a much more complex role than they previously imagined.
Researchers previously thought that meltwater simply lubricated ice against the bedrock, speeding the flow of glaciers out to sea.
Now, new studies have revealed that the effect of meltwater on acceleration and ice loss -- through fast-moving outlet glaciers that connect the inland ice sheet to the ocean -- is much more complex. This is because a kind of plumbing system evolves over time at the base of the ice, expanding and shrinking with the volume of meltwater.
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“We’ve come to realize that sub-glacial meltwater is not responsible for the big accelerations that we’ve seen for the last ten years,” Howat said. “Changes in the glacial fronts, where the ice meets the ocean, are the real key.”
“That doesn’t mean that meltwater is not important,” he continued. “It plays a role along these glacial fronts -- it’s just a very complex role, one that makes it hard for us to predict the future.”
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