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Published Online September 23, 2004 Science
DOI: 10.1126/science.1099650
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Reports
Submitted on April 27, 2004
Accepted on September 9, 2004
Accelerated Sea-Level Rise from West Antarctica
R. Thomas 1*,
E. Rignot 2,
G. Casassa 3,
P. Kanagaratnam 4,
C. Acuña 3,
T. Akins 4,
H. Brecher 5,
E. Frederick 6,
P. Gogineni 4,
W. Krabill 7,
S. Manizade 6,
H. Ramamoorthy 4,
A. Rivera 8,
R. Russell 6,
J. Sonntag 6,
R. Swift 6,
J. Yungel 6,
J. Zwally 7
1 EG&G Inc., NASA Goddard Space Flight Center (GSFC)/Wallops Flight Facility (WFF), Building N-159, Wallops Island, VA 23337, USA; Centro de Estudios Científicos (CECS), Avenida Arturo Prat 514, Casilla 1469, Valdivia, Chile.
2 Centro de Estudios Científicos (CECS), Avenida Arturo Prat 514, Casilla 1469, Valdivia, Chile; Jet Propulsion Laboratory (JPL), 4800 Oak Grove Drive, Pasadena, CA 91109, USA.
3 Centro de Estudios Científicos (CECS), Avenida Arturo Prat 514, Casilla 1469, Valdivia, Chile.
4 Radar Systems and Remote Sensing Laboratory, University of Kansas, Lawrence, KS 66045, USA.
5 Byrd Polar Research Center, Ohio State University, Columbus, OH 43210, USA.
6 EG&G Inc., NASA Goddard Space Flight Center (GSFC)/Wallops Flight Facility (WFF), Building N-159, Wallops Island, VA 23337, USA.
7 Code 972, NASA-GSFC, Greenbelt, MD 20771, USA.
8 Centro de Estudios Científicos (CECS), Avenida Arturo Prat 514, Casilla 1469, Valdivia, Chile; Departamento de Geografía, Universidad de Chile, Casilla 3387, Santiago, Chile.
* To whom correspondence should be addressed.
R. Thomas , E-mail: thomas{at}osb.wff.nasa.gov
Recent aircraft and satellite laser-altimeter surveys of the Amundsen Sea sector of West Antarctica show that local glaciers are discharging about 250 cubic km per year of ice to the ocean, almost 60% more than is accumulated within their catchment basins, and sufficient to raise sea level by more than 0.2 mm per year. Glacier thinning rates near the coast for 2002-03 are much larger than those observed during the 1990s. Most of these glaciers flow into floating ice shelves over bedrock up to hundreds of meters deeper than previous estimates, providing exit routes for ice from further inland if ice-sheet collapse is underway.
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