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The Antarctica component of postglacial rebound model ICE-6G_C (VM5a) based on GPS positioning, exposure age dating of ice thicknesses, and relative sea level histories
Geophysical Journal International · 2014 · Vol. 198(1) · pp. 537–563
Donald F. Argus✉(California Institute of Technology)W. R. Peltier(University of Toronto)R. Drummond(University of Toronto)A. W. Moore(California Institute of Technology)
Abstract
A new model of the deglaciation history of Antarctica over the past 25 kyr has been developed, which we refer to herein as ICE-6G_C (VM5a). This revision of its predecessor ICE-5G (VM2) has been constrained to fit all available geological and geodetic observations, consisting of:
Geology and Paleoclimatology ResearchCryospheric studies and observationsGeophysics and Gravity MeasurementsGeologyDeglaciationRadiocarbon datingHolocenePost-glacial reboundIce shelfLast Glacial MaximumBayGlacierIce sheet
Funding
- National Aeronautics and Space Administration
- California Institute of Technology
- Compute Canada
- University of Toronto
- National Oceanic and Atmospheric Administration
- Jet Propulsion Laboratory
- Natural Sciences and Engineering Research Council of Canada
Citations
555
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21.09
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89
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100%
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References
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Geophysical Journal International · 2012 · 611 citations
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Quaternary Science Reviews · 2006 · 1,015 citations
Global Mapping Function (GMF): A new empirical mapping function based on numerical weather model data
Geophysical Research Letters · 2006 · 1,493 citations
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