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Snowfall-Driven Growth in East Antarctic Ice Sheet Mitigates Recent Sea-Level Rise
Curt H. Davis,1*Yonghong Li,1Joseph R. McConnell,2Markus M. Frey,3Edward Hanna4
Satellite radar altimetry measurements indicate that the EastAntarctic ice-sheet interior north of 81.6°S increased inmass by 45 ± 7 billion metric tons per year from 1992to 2003. Comparisons with contemporaneous meteorological modelsnowfall estimates suggest that the gain in mass was associatedwith increased precipitation. A gain of this magnitude is enoughto slow sea-level rise by 0.12 ± 0.02 millimeters peryear.
1 Department of Electrical and Computer Engineering, University of MissouriColumbia, Columbia, MO 65211, USA. 2 Desert Research Institute, University and Community College System of Nevada, Reno, NV 89512, USA. 3 Department of Hydrology and Water Resources, University of Arizona, Tucson, AZ 85721, USA. 4 Department of Geography, University of Sheffield, Sheffield S10 2TN, UK.
* To whom correspondence should be addressed. E-mail: davisch{at}missouri.edu
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