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Published Online June 6, 2002 Science
DOI: 10.1126/science.1072708
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Research Articles
Submitted on April 9, 2002
Accepted on May 30, 2002
Surface Melt-Induced Acceleration of Greenland Ice-Sheet Flow
H. Jay Zwally 1*,
Waleed Abdalati 2,
Tom Herring 3,
Kristine Larson 4,
Jack Saba 5,
Konrad Steffen 6
1 Oceans and Ice Branch, Code 971, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA.
2 Code YS, NASA Headquarters, 300 E Street, SW, Washington, DC 20546, USA.
3 Department of Earth, Atmospheric, and Planetary Sciences, MIT Room 54-618, 77 Massachusetts Avenue, Cambridge, MA 02139, USA.
4 Department of Aerospace Engineering Sciences, University of Colorado, Boulder, CO 80309, USA.
5 Raytheon Inc., Code 971, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA.
6 CIRES, University of Colorado, CB 216, Boulder, CO 80309, USA.
* To whom correspondence should be addressed. E-mail: jay.zwally{at}gsfc.nasa.gov.
Ice flow at a location in the equilibrium zone of the west-central Greenland ice sheet accelerates above the mid-winter average rate of 31.3 cm/day during periods of summer melting. The near coincidence of the ice acceleration with the duration of surface melting, followed by deceleration after the melting ceases, indicates that glacial sliding is enhanced by rapid migration of surface melt water to the ice-bedrock interface. Interannual variations in the ice acceleration are correlated with variations in the intensity of the surface melting, from a 1.5 cm/day velocity increase during the low-melt summer of 1996, to 3.8 cm/day in the average-melt summer of 1997, and to 8.8 cm/day and 7.3 cm/day increases during the high-melt summers of 1998 and 1999. The indicated coupling between surface melting and ice-sheet flow provides a mechanism for rapid large-scale dynamic response of ice sheets to climate warming.
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