-Caveat Lector-

-------- Original Message --------
Subject: Polar Ice Sheet Shows Shrinkage
Date: Sat, 3 Feb 2001 00:12:17 -0600 (CST)
From: Mark Graffis <[EMAIL PROTECTED]>
Organization: ?
To: undisclosed-recipients:;

   Thursday February 1 3:47 PM ET

   By PAUL RECER, AP Science Writer

   WASHINGTON (AP) - Scientists have worried for decades that the
   Antarctic ice sheet was shrinking, threatening a global rise in sea
   level. Now, satellite studies show that about 7.5 cubic miles of ice
   have eroded from a key area in just eight years.

   Melting of that much ice doesn't mean that it is time to get into
   boats, said one researcher, but the finding may be a ``yellow warning
   flag'' that confirms long-term changes are under way in the ice fields
   covering the South Polar region.

   The study, which appears Friday in the journal Science, involved
   altitude measurements of the West Antarctica Ice Sheet, the smaller of
   two major ice sheets. It covers 740,000 square miles of the frozen
   continent.

   Based on satellite measurements, said Andrew Shepherd, a University
   College London geologist and first author of the study, it appears
   that since 1992 the ice sheet has lost ice principally through the
   speeded-up movement of the Pine Island Glacier, an ice stream that
   drains about a third of the ice sheet.

   ``The Pine Island Glacier is key,'' said Shepherd. ``It is totally
   exposed to the sea, and people have identified it as the weak
   underbelly of the West Antarctica Ice Sheet.''

   Melting of the entire sheet theoretically could cause a global sea
   level rise of 25 to 45 feet, but Shepherd said that at the present
   rate of change it would take centuries for the Pine Island Glacier,
   which is only about 10 percent of the ice sheet, to affect sea level
   seriously.

   Jane Ferrigno, a U.S. Geologic Survey geologist and polar ice expert,
   said a speedup of the Pine Island Glacier, as reported by Shepherd and
   his co-authors, could foreshadow continuing changes of the West
   Antarctica Ice Sheet's ice levels.

   The glacier ``is moving faster than we thought,'' Ferrigno said.
   ``This doesn't mean it could have an effect on coastal areas around
   the world within the next few decades, but this is a yellow warning
   flag. This is an area that should be watched carefully.''

   Shepherd said eight years of satellite data show a steady trend of
   ice-sheet shrinkage, with most of the decline coming in the Pine
   Island Glacier system, which drains an area about the size of the
   Mississippi River basin.

   The Pine Island Glacier thinned by 30 to 36 feet during those eight
   years, and the glacier's grounding line - the point where sea water
   undercuts the main stem of the glacier - has pushed inland by about
   three miles.

   ``The thinning is 10 times greater than the rate of snowfall in the
   basin,'' said Shepherd. ``The speed of the glacier means that much
   more mass is going out (through melting and breaking off of icebergs)
   than is coming in.''

   Shepherd said if the present rate of change continues, the main stem
   of the Pine Island Glacier will be undercut by the sea and lifted up
   in about 600 years. When the glacier floats, it would cause a dramatic
   shift in sea level, he said.

   Understanding how fast the Pine Island Glacier is moving and the
   effect of this motion on the total West Antarctica Ice Sheet ``is of
   considerable importance'' in predicting what will happen to the ice in
   Antarctica, Ferrigno said. She said the work by Shepherd and his
   co-authors adds new data for an area of the polar continent that was
   virtually unknown before.

   Antarctica contains about 7.2 million cubic miles of ice, about 84
   percent of all the glacial ice on Earth, according to the USGS.
   Melting all the Antarctica ice would cause a global sea level rise of
   about 240 feet. Such a rise would flood virtually all the world's
   coastal areas and drown many islands.

   -

   On the Net: Science journal: [25]http://www.eurekalert.org

   USGS:
   [26]http://terraweb.wr.usgs.gov/TRS/projects/Antarctica/AVHRR.html

   USGS site for glacial volume, sea-level rise potential:
   [27]http://pubs.usgs.gov/factsheet/fs133-99/gl-vol.html

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