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			by Jenny Hogan 
			
			Exeter  
			
			13:38 02 February 2005  
			
			NewScientist.com news service  
  
			
			The massive west Antarctic ice sheet, 
			previously assumed to be stable, is starting to collapse, scientists 
			warned on Tuesday. 
			 
			Antarctica contains more than 90% of the world's ice, and the loss 
			of any significant part of it would cause a substantial sea level 
			rise. Scientists used to view Antarctica as a "slumbering giant", 
			said Chris Rapley, from the British Antarctic Survey, but now he 
			sees it as an "awakened giant".  
			 
			Rapley presented measurements of the ice sheet at a major climate 
			conference in Exeter, UK. Glaciers on the Antarctic peninsula, which 
			protrudes from the continent to the north, were already known to be 
			retreating. But the data Rapley presented show that glaciers within 
			the much larger west Antarctic Ice sheet are also starting to 
			disappear. 
			 
			If the ice on the peninsula melts entirely it will raise global sea 
			levels by 0.3 meters, and the west Antarctic ice sheet contains 
			enough water to contribute meters more. The last report of the 
			Intergovernmental Panel on Climate Change, published in 2001, said 
			that collapse of this ice sheet was unlikely during the 21st 
			century. That may now need to be reassessed, Rapley warned. 
  
			
			 
			Cork from a 
			bottle 
			
			 
			Changes on the peninsula, where 75% of the 400 mountain glaciers are 
			in retreat, have provided new insights into the ways that ice sheets 
			may disintegrate.  
			 
			In March 2002, a huge floating ice shelf known as Larsen B shattered 
			into icebergs. This turned out to have an effect akin to pulling a 
			cork from a bottle. With Larsen B no longer impeding movement, the 
			ice floes that fed the shelf began moving faster towards the sea and 
			started to thin. The finding took scientists by surprise when 
			revealed in September 2004 and now modellers are now working to 
			include such mechanisms in their predictions. 
			 
			Climate records derived from the analysis of sediments show that ice 
			shelves off the peninsula have been absent in several earlier eras, 
			when natural variability warmed the world. But the break-up is 
			affecting ice closer to the pole than ever recorded, said Rapley. 
			 
			
				
				"It's like the Heineken effect," he said, referring to the beer 
			adverts that claim Heineken "reaches the parts other beers cannot 
			reach".  
			 
			
			Indications that climate change may be affecting the west Antarctic 
			ice sheet comes from three glaciers, including Pine Island and 
			Thwaites. Data reveal they are losing more ice - mainly through the 
			calving of icebergs - than is being replaced by snowfall. According 
			to a preliminary analysis, the difference between the mass lost and 
			mass replaced is about 60%. 
			 
			Whether the loss of mass by the glaciers is due to natural variation 
			or is caused by human-influenced warming of the oceans is not known 
			for sure. Scientists are now making more field measurements to 
			assess the causes, but warming is a likely culprit, said Rapley: 
			 
			
				
				"The fact that three of them are simultaneously accelerating 
			suggests that is the case."  
			 
			
			The melting of these three glaciers 
			alone is contributing an estimated 0.24 millimeters per year to sea 
			level.  
  
			
			
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