Brief communication

The global signature of post-1900 land ice wastage on vertical land motion

Journal Article (2017)
Author(s)

R.E.M. Riva (TU Delft - Physical and Space Geodesy)

T. Frederikse (TU Delft - Physical and Space Geodesy)

Matt A. King (University of Tasmania)

Ben Marzeion (University of Bremen)

M. R. R. Van Den Broeke (Universiteit Utrecht)

Research Group
Physical and Space Geodesy
Copyright
© 2017 R.E.M. Riva, T. Frederikse, A. Matt King, Ben Marzeion, Michiel R. van den Broeke
DOI related publication
https://doi.org/10.5194/tc-11-1327-2017
More Info
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Publication Year
2017
Language
English
Copyright
© 2017 R.E.M. Riva, T. Frederikse, A. Matt King, Ben Marzeion, Michiel R. van den Broeke
Research Group
Physical and Space Geodesy
Issue number
3
Volume number
11
Pages (from-to)
1327-1332
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Abstract

Melting glaciers, ice caps and ice sheets have made an important contribution to sea-level rise through the last century. Self-attraction and loading effects driven by shrinking ice masses cause a spatially varying redistribution of ocean waters that affects reconstructions of past sea level from sparse observations. We model the solid-earth response to ice mass changes and find significant vertical deformation signals over large continental areas. We show how deformation rates have been strongly varying through the last century, which implies that they should be properly modelled before interpreting and extrapolating recent observations of vertical land motion and sea-level change.