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State-of-the-art in studies of glacial isostatic adjustment for the British Isles: a literature review

Published online by Cambridge University Press:  17 October 2016

Julia Stockamp ,
Paul Bishop ,
Zhenhong Li ,
Elizabeth J Petrie ,
Jim Hansom  and
Alistair Rennie
Julia Stockamp
Affiliation:
School of Geographical and Earth Sciences, University of Glasgow, Glasgow G12 8QQ, UK. Email: [email protected]; [email protected]; [email protected]; [email protected] COMET, School of Civil Engineering and Geosciences, Newcastle University, Newcastle upon Tyne NE1 7RU, UK. Email: [email protected]
Paul Bishop
Affiliation:
School of Geographical and Earth Sciences, University of Glasgow, Glasgow G12 8QQ, UK. Email: [email protected]; [email protected]; [email protected]; [email protected]
Zhenhong Li
Affiliation:
COMET, School of Civil Engineering and Geosciences, Newcastle University, Newcastle upon Tyne NE1 7RU, UK. Email: [email protected]
Elizabeth J Petrie
Affiliation:
School of Geographical and Earth Sciences, University of Glasgow, Glasgow G12 8QQ, UK. Email: [email protected]; [email protected]; [email protected]; [email protected]
Jim Hansom
Affiliation:
School of Geographical and Earth Sciences, University of Glasgow, Glasgow G12 8QQ, UK. Email: [email protected]; [email protected]; [email protected]; [email protected]
Alistair Rennie
Affiliation:
Scottish Natural Heritage, Leachkin Road, Inverness IV3 8NW, UK. Email: [email protected]
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Abstract

Understanding the effects of glacial isostatic adjustment (GIA) of the British Isles is essential for the assessment of past and future sea-level trends. GIA has been extensively examined in the literature, employing different research methods and observational data types. Geological evidence from palaeo-shorelines and undisturbed sedimentary deposits has been used to reconstruct long-term relative sea-level change since the Last Glacial Maximum. This information derived from sea-level index points has been employed to inform empirical isobase models of the uplift in Scotland using trend surface and Gaussian trend surface analysis, as well as to calibrate more theory-driven GIA models that rely on Earth mantle rheology and ice sheet history. Furthermore, current short-term rates of GIA-induced crustal motion during the past few decades have been measured using different geodetic techniques, mainly continuous GPS (CGPS) and absolute gravimetry (AG). AG-measurements are generally employed to increase the accuracy of the CGPS estimates. Synthetic aperture radar interferometry (InSAR) looks promising as a relatively new technique to measure crustal uplift in the northern parts of Great Britain, where the GIA-induced vertical land deformation has its highest rate. This literature review provides an in-depth comparison and discussion of the development of these different research approaches.

Keywords

Absolute gravitycontinuous GPSGIA modellingmantle rheologypostglacial reboundrelative sea-level changeSAR interferometryScotland
Type
Articles
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 106 , Issue 3 , September 2015 , pp. 145 - 170
Copyright
Copyright © The Royal Society of Edinburgh 2016 

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