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Science 21 July 2000: Vol. 289. no. 5478, pp. 426 - 428 DOI: 10.1126/science.289.5478.426
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Reports
Mass Balance of the Greenland Ice Sheet at High Elevations
R. Thomas,1*
T. Akins,2
B. Csatho,3
M. Fahnestock,4
P. Gogineni,5
C. Kim,3
J. Sonntag1
Comparison of ice discharge from higher elevation areas of the
entire Greenland Ice Sheet with total snow accumulation gives estimates
of ice thickening rates over the past few decades. On average, the
region has been in balance, but with thickening of 21 centimeters per
year in the southwest and thinning of 30 centimeters per year in the
southeast. The north of the ice sheet shows less variability, with
average thickening of 2 centimeters per year in the northeast and
thinning of about 5 centimeters per year in the northwest. These
results agree well with those from repeated altimeter surveys, except
in the extreme south, where we find substantially higher rates of both
thickening and thinning.
1 EG&G Services, Wallops Flight Facility,
Building N-159, Wallops Island, VA 23337, USA.
2 Jet
Propulsion Laboratory, M/S 300-325, 4800 Oak Grove Drive, Pasadena, CA
91109, USA.
3 Byrd Polar Research Center, Ohio State
University, Columbus, OH 42310, USA.
4 ESSIC,
University of Maryland, College Park, MD 20742, USA.
5 Radar Systems and Remote Sensing Laboratory,
University of Kansas, Lawrence, KS 66045, USA.
*
To whom correspondence should be addressed.
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THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
- Kinematic Constraints on Glacier Contributions to 21st-Century Sea-Level Rise.
- W. T. Pfeffer, J. T. Harper, and S. O'Neel (2008)
Science
321, 1340-1343
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- Greenland Ice Sheet: High-Elevation Balance and Peripheral Thinning.
- W. Krabill, W. Abdalati, E. Frederick, S. Manizade, C. Martin, J. Sonntag, R. Swift, R. Thomas, W. Wright, and J. Yungel (2000)
Science
289, 428-430
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