The rate of glaciers and basins dumping ice into the ocean have increased over the past decade, according to the study published in yesterday's issue of the journal Nature Geoscience.
(Related: "Small Melting Glaciers Will Speed Sea Level Rise, Study Says" [July 19, 2007].)
The researchers used measurements from European, Canadian, and Japanese satellites, which scanned about 85 percent of Antarctica's coasts from 1996 to 2006.
The results showed that most of the ice is being lost through a few fast-flowing glaciers and basins.
"We can pinpoint with a lot of precision exactly where the losses are taking place and the characteristics of those losses," Bamber said.
The new study also covers a longer period of time than past research efforts.
The research method, called radar inferometry, measured how quickly ice was flowing. It also captured how thick the ice was at the grounding point, which is where the ocean causes ice to lift off the land and start floating.
The "most likely explanation" for the increased ice loss is that warming waters are melting away ice at the grounding point, according to Bamber.
"That's causing the buttressing effect of the ice shelves to be less [effective], and that's allowing the glaciers to flow faster into the ocean," he said.
Eric Rignot of NASA's Jet Propulsion Laboratory in Pasadena, California, is the lead study author.
"The climate models neglected changes in speeds of glaciers," Rignot said. "It turns out that is the main control on the ice mass balance."
"The ice loss we see is going to continue, and it's going to grow" because the oceans around Antarctica are expected to warm, Rignot added.
The new study "tells us that the glaciers are losing more mass, which is one part of the total mass change," said Andrew Shepherd of the University of Edinburgh in Scotland.
However Shepherd, who was not involved in the new research, argued that it's not clear whether Antarctica is actually losing more ice now than it did ten years ago, and what the future will hold.
"What we still don't know is the total mass change [over that period], because we don't know how much extra snow has fallen there," Shepherd said.
This snowfall in inland Antarctica is the main unknown in these estimates, Bamber agrees. But they say their method has been able to get a better estimate of the snowfall than earlier studies. (Related: "Antartica Snowfall Not Curbing Sea Level Rise, Study Says" [August 11, 2006].)
The problem is that people rarely go to the interior of Antarctica, and measurements of snowfall are sparse.
But an upcoming project will take measurements on the ground and should help settle the matter, Bamber said. Also, improving how climate models treat the dynamic nature of glaciers and ice sheets is crucial, experts say.
The head of the UN Intergovernmental Panel of Climate Change recently called for improvements in estimates of ice loss in Greenland and Antarctica.
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