Glacio-Isostatic Adjustment is a geophysical process that describes the delayed viscoelastic response of the Earth's lithosphere and mantle to the redistribution of ice and ocean mass during glacial cycles, manifested as vertical crustal movements and associated changes in relative sea level.
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A Reconciled Estimate of Ice-Sheet Mass Balance
Andrew Shepherd, Erik R. Ivins, A Geruo et al. · Science · 2012 · 1.6K citations · Full text
Mass balance of the Antarctic Ice Sheet from 1992 to 2017
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University of Toronto
Toronto, Canada
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Durham University
Durham, United Kingdom
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Delft University of Technology
Delft, The Netherlands
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Planetary Science Institute
Tucson, United States
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GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
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University of Calgary
Calgary, Canada
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Cambridge, United States
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37 publications · 2K citations
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24 publications · 2.1K citations
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- Earth and Planetary Science Letters
17 publications · 940 citations
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