Abstract
Accurate quantification of Antarctic ice-sheet mass balance and its contribution to global sea-level rise remains challenging, because in situ measurements over both space and time are sparse. Satellite remote-sensing data of ice elevations and ice motion show significant ice loss in the range of â31 to â196âGtâyrâ1 in West Antarctica in recent years1,2,3,4, whereas East Antarctica seems to remain in balance or slightly gain mass1,2,4, with estimated rates of mass change in the range of â4 to 22âGtâyrâ1. The Gravity Recovery and Climate Experiment5 (GRACE) offers the opportunity of quantifying polar ice-sheet mass balance from a different perspective6,7. Here we use an extended record of GRACE data spanning the period April 2002 to January 2009 to quantify the rates of Antarctic ice loss. In agreement with an independent earlier assessment4, we estimate a total loss of 190±77âGtâyrâ1, with 132±26âGtâyrâ1 coming from West Antarctica. However, in contrast with previous GRACE estimates, our data suggest that East Antarctica is losing mass, mostly in coastal regions, at a rate of â57±52âGtâyrâ1, apparently caused by increased ice loss since the year 2006.
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Acknowledgements
This research was supported by NASA GRACE Science Program (NNX08AJ84G), NASA PECASE award (NNG04G060G) and NSF International Polar Year Program (ANT-0632195).
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J.L.C. planned analyses, acquired and prepared data, implemented forward modelling and wrote the paper. C.R.W., D.B. and B.D.T. analysed the data and results.
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Chen, J., Wilson, C., Blankenship, D. et al. Accelerated Antarctic ice loss from satellite gravity measurements. Nature Geosci 2, 859â862 (2009). https://doi.org/10.1038/ngeo694
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DOI: https://doi.org/10.1038/ngeo694
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