Dr Grace Nield grace.a.nield@durham.ac.uk
Assistant Professor
Rapid bedrock uplift in the Antarctic Peninsula explained by viscoelastic response to recent ice unloading
Nield, G.A.; Barletta, V.R.; Bordoni, A.; King, M.A.; Whitehouse, P.L.; Clarke, P.J.; Domack, E.; Scambos, T.A.; Berthier, E.
Authors
V.R. Barletta
A. Bordoni
M.A. King
Professor Pippa Whitehouse pippa.whitehouse@durham.ac.uk
Professor
P.J. Clarke
E. Domack
T.A. Scambos
E. Berthier
Abstract
Since 1995 several ice shelves in the Northern Antarctic Peninsula have collapsed and triggered ice-mass unloading, invoking a solid Earth response that has been recorded at continuous GPS (cGPS) stations. A previous attempt to model the observation of rapid uplift following the 2002 breakup of Larsen B Ice Shelf was limited by incomplete knowledge of the pattern of ice unloading and possibly the assumption of an elastic-only mechanism. We make use of a new high resolution dataset of ice elevation change that captures ice-mass loss north of 66°S to first show that non-linear uplift of the Palmer cGPS station since 2002 cannot be explained by elastic deformation alone. We apply a viscoelastic model with linear Maxwell rheology to predict uplift since 1995 and test the fit to the Palmer cGPS time series, finding a well constrained upper mantle viscosity but less sensitivity to lithospheric thickness. We further constrain the best fitting Earth model by including six cGPS stations deployed after 2009 (the LARISSA network), with vertical velocities in the range 1.7 to 14.9 mm/yr. This results in a best fitting Earth model with lithospheric thickness of 100–140 km and upper mantle viscosity of View the MathML source6×1017–2×1018 Pas – much lower than previously suggested for this region. Combining the LARISSA time series with the Palmer cGPS time series offers a rare opportunity to study the time-evolution of the low-viscosity solid Earth response to a well-captured ice unloading event.
Citation
Nield, G., Barletta, V., Bordoni, A., King, M., Whitehouse, P., Clarke, P., …Berthier, E. (2014). Rapid bedrock uplift in the Antarctic Peninsula explained by viscoelastic response to recent ice unloading. Earth and Planetary Science Letters, 397, 32-41. https://doi.org/10.1016/j.epsl.2014.04.019
Journal Article Type | Article |
---|---|
Acceptance Date | Apr 9, 2014 |
Online Publication Date | May 5, 2014 |
Publication Date | Jul 1, 2014 |
Deposit Date | May 16, 2014 |
Publicly Available Date | May 21, 2014 |
Journal | Earth and Planetary Science Letters |
Print ISSN | 0012-821X |
Publisher | Elsevier |
Peer Reviewed | Peer Reviewed |
Volume | 397 |
Pages | 32-41 |
DOI | https://doi.org/10.1016/j.epsl.2014.04.019 |
Keywords | Antarctic Peninsula, Larsen B, Ice-mass loss, Viscoelastic uplift, GPS, Upper mantle viscosity. |
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Publisher Licence URL
http://creativecommons.org/licenses/by/3.0/
Copyright Statement
This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/3.0/)
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