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Published Online October 19, 2006
Science DOI: 10.1126/science.1130776

Reports

Submitted on June 2, 2006
Accepted on October 10, 2006

Recent Greenland Ice Mass Loss by Drainage System from Satellite Gravity Observations

S. B. Luthcke 1*, H. J. Zwally 2, W. Abdalati 2, D. D. Rowlands 1, R. D. Ray 1, R. S. Nerem 3, F. G. Lemoine 1, J. J. McCarthy 4, D. S. Chinn 4

1 Planetary Geodynamics Laboratory, Code 698
2 Cryospheric Sciences Branch, Code 614.1, NASA Goddard Space Flight Center Greenbelt, MD 20771 USA.
3 Colorado Center for Astrodynamics Research, Cooperative Institute for Research in Environmental Sciences, Dept of Aerospace Engineering Sciences, The University of Colorado, Boulder, CO 80309 USA.
4 Science Division, SGT Inc., Greenbelt, MD 20770 USA.

* To whom correspondence should be addressed.
S. B. Luthcke , E-mail: Scott.B.Luthcke{at}nasa.gov

Mass changes of the Greenland ice sheet resolved by drainage system (DS) regions are derived from a local mass concentration analysis of the GRACE mission gravity observations. During 2003-2005, the ice sheet lost 101±16 Gt/yr with a gain of 54 Gt/yr above 2000 m and a loss of 155 Gt/yr at lower elevations. The lower elevations show a large seasonal cycle with mass losses during summer melting followed by gains from fall through spring. The overall rate of loss reflects a considerable change in trend (-113 ± 17 Gt/yr) from a near balance of the 1990's, but is smaller than some other recent estimates.



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