Viscous gravitational relaxation

This paper is concerned with a detailed examination of the response of Maxwell models of the planet to surface mass loads. Particular attention is devoted to an examination of the factors which determine the isostatic response since the understanding of this response is crucial in a number of differ...

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Published in:Geophysical Journal International
Main Authors: Wu, Patrick, Peltier, W. R.
Format: Text
Language:English
Published: Oxford University Press 1982
Subjects:
Online Access:http://gji.oxfordjournals.org/cgi/content/short/70/2/435
https://doi.org/10.1111/j.1365-246X.1982.tb04976.x
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spelling fthighwire:oai:open-archive.highwire.org:gji:70/2/435 2023-05-15T16:40:54+02:00 Viscous gravitational relaxation Wu, Patrick Peltier, W. R. 1982-08-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/70/2/435 https://doi.org/10.1111/j.1365-246X.1982.tb04976.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/70/2/435 http://dx.doi.org/10.1111/j.1365-246X.1982.tb04976.x Copyright (C) 1982, Oxford University Press Articles TEXT 1982 fthighwire https://doi.org/10.1111/j.1365-246X.1982.tb04976.x 2012-11-23T22:12:41Z This paper is concerned with a detailed examination of the response of Maxwell models of the planet to surface mass loads. Particular attention is devoted to an examination of the factors which determine the isostatic response since the understanding of this response is crucial in a number of different geodynamic problems. One particular example which we discuss in detail is concerned with the prediction of free air gravity anomalies produced by large-scale deglaciation events. Using the methods developed here we are able to provide the first direct assessment of the importance of initial isostatic disequilibrium on the observed relative sea-level variations and free air gravity anomalies forced by the melting of the Laurentide ice sheet. We are therefore able to estimate the extent to which such initial disequilibrium might influence the inference of mantle viscosity from isostatic adjustment data. Our calculations establish that free air gravity data, although they are sensitive to the degree of initial disequilibrium, provide an extremely high quality constraint upon the viscosity of the lower mantle. Text Ice Sheet HighWire Press (Stanford University) Geophysical Journal International 70 2 435 485
institution Open Polar
collection HighWire Press (Stanford University)
op_collection_id fthighwire
language English
topic Articles
spellingShingle Articles
Wu, Patrick
Peltier, W. R.
Viscous gravitational relaxation
topic_facet Articles
description This paper is concerned with a detailed examination of the response of Maxwell models of the planet to surface mass loads. Particular attention is devoted to an examination of the factors which determine the isostatic response since the understanding of this response is crucial in a number of different geodynamic problems. One particular example which we discuss in detail is concerned with the prediction of free air gravity anomalies produced by large-scale deglaciation events. Using the methods developed here we are able to provide the first direct assessment of the importance of initial isostatic disequilibrium on the observed relative sea-level variations and free air gravity anomalies forced by the melting of the Laurentide ice sheet. We are therefore able to estimate the extent to which such initial disequilibrium might influence the inference of mantle viscosity from isostatic adjustment data. Our calculations establish that free air gravity data, although they are sensitive to the degree of initial disequilibrium, provide an extremely high quality constraint upon the viscosity of the lower mantle.
format Text
author Wu, Patrick
Peltier, W. R.
author_facet Wu, Patrick
Peltier, W. R.
author_sort Wu, Patrick
title Viscous gravitational relaxation
title_short Viscous gravitational relaxation
title_full Viscous gravitational relaxation
title_fullStr Viscous gravitational relaxation
title_full_unstemmed Viscous gravitational relaxation
title_sort viscous gravitational relaxation
publisher Oxford University Press
publishDate 1982
url http://gji.oxfordjournals.org/cgi/content/short/70/2/435
https://doi.org/10.1111/j.1365-246X.1982.tb04976.x
genre Ice Sheet
genre_facet Ice Sheet
op_relation http://gji.oxfordjournals.org/cgi/content/short/70/2/435
http://dx.doi.org/10.1111/j.1365-246X.1982.tb04976.x
op_rights Copyright (C) 1982, Oxford University Press
op_doi https://doi.org/10.1111/j.1365-246X.1982.tb04976.x
container_title Geophysical Journal International
container_volume 70
container_issue 2
container_start_page 435
op_container_end_page 485
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