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A new global GPS data set for testing and improving modelled GIA uplift rates


Schumacher, M and King, MA and Rougier, J and Sha, Z and Khan, SA and Bamber, JL, A new global GPS data set for testing and improving modelled GIA uplift rates, Geophysical Journal International, 214, (3) pp. 2164-2176. ISSN 0956-540X (2018) [Refereed Article]


Copyright Statement

Copyright 2018 The Author(s). Published by Oxford University Press on behalf of The Royal Astronomical Society. Licensed under Creative Commons Attribution 4.0 International (CC BY 4.0)

DOI: doi:10.1093/gji/ggy235


Glacial isostatic adjustment (GIA) is the response of the solid Earth to past ice loading, primarily, since the Last Glacial Maximum, about 20 K yr BP. Modelling GIA is challenging because of large uncertainties in ice loading history and also the viscosity of the upper and lower mantle. GPS data contain the signature of GIA in their uplift rates but these also contain other sources of vertical land motion (VLM) such as tectonics, human and natural influences on water storage that can mask the underlying GIA signal. In this study, we use about 4000 GPS vertical velocities as observational estimates of global GIA uplift rates, after correcting for major elastic deformation effects. A novel fully automatic strategy is developed to postprocess the GPS time-series and to correct for non-GIA artefacts. Before estimating vertical velocities and uncertainties, we detect outliers and jumps and correct for atmospheric mass loading displacements. We correct the resulting velocities for the elastic response of the solid Earth to global changes in ice sheets, glaciers and ocean loading, as well as for changes in the Earth’s rotational pole relative to the 20th century average. We then apply a spatial median filter to remove sites where local effects are dominant to leave approximately 4000 GPS sites. The resulting novel global GPS data set shows a clean GIA signal at all post-processed stations and is therefore suitable to investigate the behavior of global GIA forward models. The results are transformed from a frame with its origin in the centre of mass of the total Earth’s system (CM) into a frame with its origin in the centre of mass of the solid Earth (CE) before comparison with 13 global GIA forward model solutions, with best fits with Pur-6- VM5 and ICE-6G predictions. The largest discrepancies for all models were identified for Antarctica and Greenland, which may be due to either uncertain mantle rheology, ice loading history/magnitude and/or GPS errors.

Item Details

Item Type:Refereed Article
Keywords:glacial isostatic adjustment, GPS, vertical velocity, forward models, GIA, GPS, inverse solutions
Research Division:Earth Sciences
Research Group:Geophysics
Research Field:Geodesy
Objective Division:Expanding Knowledge
Objective Group:Expanding knowledge
Objective Field:Expanding knowledge in the earth sciences
UTAS Author:King, MA (Professor Matt King)
ID Code:127363
Year Published:2018
Web of Science® Times Cited:24
Deposited By:Geography and Spatial Science
Deposited On:2018-07-23
Last Modified:2022-08-23
Downloads:77 View Download Statistics

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