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Growth of Greenland Ice Sheet: Interpretation
H. Jay Zwally
New Series, Vol. 246, No. 4937 (Dec. 22, 1989), pp. 1589-1591
Published by: American Association for the Advancement of Science
Stable URL: http://www.jstor.org/stable/1704666
Page Count: 3
You can always find the topics here!Topics: Ice, Ice sheets, Precipitation, Melting, Crossovers, Topographical elevation, Oceans, Antarctic regions, Mass balance, Velocity
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An observed 0.23 m/year thickening of the Greenland ice sheet indicates a 25% to 45% excess ice accumulation over the amount required to balance the outward ice flow. The implied global sea-level depletion is 0.2 to 0.4 mm/year, depending on whether the thickening is only recent (5 to 10 years) or longer term (<100 years). If there is a similar imbalance in the northern 60% of the ice-sheet area, the depletion is 0.35 to 0.7 mm/year. Increasing ice thickness suggests that the precipitation is higher than the long-term average; higher precipitation may be a characteristic of warmer climates in polar regions.
Science © 1989 American Association for the Advancement of Science