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Science

Publication date: 2012-01-01
Volume: 338 Pages: 1183 - 1189
Publisher: American Association for the Advancement of Science

Author:

Shepherd, Andrew
Ivins, Erik R ; Geruo, A ; Barletta, Valentina R ; Bentley, Mike J ; Bettadpur, Srinivas ; Briggs, Kate H ; Bromwich, David H ; Forsberg, Rene ; Galin, Natalia ; Horwath, Martin ; Jacobs, Stan ; Joughin, Ian ; King, Matt A ; Lenaerts, Jan ; Li, Jilu ; Ligtenberg, Stefan RM ; Luckman, Adrian ; Luthcke, Scott B ; McMillan, Malcolm ; Meister, Rakia ; Milne, Glenn ; Mouginot, Jeremie ; Muir, Alan ; Nicolas, Julien P ; Paden, John ; Payne, Antony J ; Pritchard, Hamish ; Rignot, Eric ; Rott, Helmut ; Sorensen, Louise Sandberg ; Scambos, Ted A ; Scheuchl, Bernd ; Schrama, Ernst JO ; Smith, Ben ; Sundal, Aud V ; van Angelen, Jan H ; van de Berg, Willem J ; van den Broeke, Michiel R ; Vaughan, David G ; Velicogna, Isabella ; Wahr, John ; Whitehouse, Pippa L ; Wingham, Duncan J ; Yi, Donghui ; Young, Duncan ; Zwally, H Jay

Keywords:

Science & Technology, Multidisciplinary Sciences, Science & Technology - Other Topics, PINE ISLAND GLACIER, RELATIVE SEA-LEVEL, ISOSTATIC-ADJUSTMENT, ANTARCTIC PENINSULA, WEST ANTARCTICA, GREENLAND, MODEL, CLIMATE, SURFACE, SHELF, Antarctic Regions, Climate Change, Geographic Information Systems, Greenland, Ice Cover, General Science & Technology

Abstract:

We combined an ensemble of satellite altimetry, interferometry, and gravimetry data sets using common geographical regions, time intervals, and models of surface mass balance and glacial isostatic adjustment to estimate the mass balance of Earth's polar ice sheets. We find that there is good agreement between different satellite methods--especially in Greenland and West Antarctica--and that combining satellite data sets leads to greater certainty. Between 1992 and 2011, the ice sheets of Greenland, East Antarctica, West Antarctica, and the Antarctic Peninsula changed in mass by -142 ± 49, +14 ± 43, -65 ± 26, and -20 ± 14 gigatonnes year(-1), respectively. Since 1992, the polar ice sheets have contributed, on average, 0.59 ± 0.20 millimeter year(-1) to the rate of global sea-level rise.