Mass balance of the Antarctic Ice Sheet from 1992 to 2017
Wouters, Bert
- 1Univ Leeds
- 2National Aeronautics & Space Administration (NASA)
- 3University of California System
- 4University of Washington
- 5Utrecht University
- 6Durham University
- 7Communaute Universite Grenoble Alpes
- 8University of Bristol
- 9University of Colorado System
- 10University of Liege
- 11Geological Survey Of Denmark & Greenland
- 12State University of New York (SUNY) System
- 13Technical University of Denmark
- 14Spatial Geophys & Oceanog Studies Lab
- 15State University System of Florida
- 16University of Texas System
- 17University of London
- 18Technische Universitat Dresden
- 19University System of Georgia
- 20University of Lincoln
- 21University of Arizona
- 22Helmholtz Association
- 23Technical University of Munich
- 24Danish Meteorological Institute DMI
- 25Memorial University Newfoundland
- 26Istituto Nazionale Geofisica e Vulcanologia (INGV)
- 27
- 28Newcastle University - UK
- 29isardSAT
- 30ENVEO
- 31University of Toronto
- 32University of Bonn
- 33Delft University of Technology
- 34Seoul National University (SNU)
- 35University of Urbino
- 36University of Stuttgart
Journal
Nature
ISSN
0028-0836
1476-4687
Open Access
green
Volume
558
Start page
219
End page
222
The Antarctic Ice Sheet is an important indicator of climate change and driver of sea-level rise. Here we combine satellite observations of its changing volume, flow and gravitational attraction with modelling of its surface mass balance to show that it lost 2,720 +/- 1,390 billion tonnes of ice between 1992 and 2017, which corresponds to an increase in mean sea level of 7.6 +/- 3.9 millimetres (errors are one standard deviation). Over this period, ocean-driven melting has caused rates of ice loss from West Antarctica to increase from 53 +/- 29 billion to 159 +/- 26 billion tonnes per year; ice-shelf collapse has increased the rate of ice loss from the Antarctic Peninsula from 7 +/- 13 billion to 33 +/- 16 billion tonnes per year. We find large variations in and among model estimates of surface mass balance and glacial isostatic adjustment for East Antarctica, with its average rate of mass gain over the period 1992-2017 (5 +/- 46 billion tonnes per year) being the least certain.
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Type
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