Fears that global sea levels this century may rise faster and further than expected are supported by a study showing that 300 glaciers in Antarctica have begun to move more quickly into the ocean.
Scientists believe that the accelerated movement of glaciers in the Antarctic Peninsula indicates a dramatic shift in the way melting ice around the world contributes to overall increases in global sea levels.
Instead of simply adding huge volumes of meltwater to the sea, scientists have found rising temperatures are causing glaciers as far apart as Alaska, Greenland and now Antarctica to break up and slip into the ocean at a faster rate than expected.
The findings will raise concerns within the UN's Intergovernmental Panel on Climate Change (IPCC) which, earlier this year, downplayed the so-called "dynamic" nature of melting glaciers - when rising temperatures cause them to break up quickly rather than simply melt slowly.
Using radar images taken between 1993 and 2003, scientists at the British Antarctic Survey in Cambridge mapped a 12 per cent increase in the average rate of movement of more than 300 glaciers in the Antarctic Peninsula over the period.
The scientists believe that their findings are among the first to suggest that as glaciers being to melt they experience a physical transformation that causes an acceleration in their movement into the sea.
"We're only just now getting to grips with just how big these dynamic processes may be. There are still a lot of surprises out there," said David Vaughan, a glaciologist at the British Antarctic Survey and a co-author of the study.
"It is yet another example of how subpolar glaciers are responding very quickly to climate change because they are close to the temperature transition from ice to water," Dr Vaughan said.
"Scientists want to know why these things are happening because that's the route to the prediction of future sea levels."
In its fourth report published in February, the IPCC said sea levels this century could rise by between 20 cms and 43cms but it accepted that this could be a serious underestimate if ice sheets and glaciers undergo the sort of dynamic changes that existing computer models do not take fully into account.,,,
Tuesday, June 05, 2007
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