The stability of a viscous till sheet coupled with ice flow, considered at wavelengths less than the ice thickness

Abstract A perturbation method is used to analyse the stability of a thin till layer overlain by a deep ice layer. Ice is modelled as a linearly viscous fluid, while the till viscosity has power-law dependence on stress and effective pressure. A linearized set of equations yields descriptions of the...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Author: Hindmarsh, Richard C. A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1998
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000002628
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000002628
id crcambridgeupr:10.1017/s0022143000002628
record_format openpolar
spelling crcambridgeupr:10.1017/s0022143000002628 2024-05-19T07:42:09+00:00 The stability of a viscous till sheet coupled with ice flow, considered at wavelengths less than the ice thickness Hindmarsh, Richard C. A. 1998 http://dx.doi.org/10.1017/s0022143000002628 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000002628 en eng Cambridge University Press (CUP) Journal of Glaciology volume 44, issue 147, page 285-292 ISSN 0022-1430 1727-5652 journal-article 1998 crcambridgeupr https://doi.org/10.1017/s0022143000002628 2024-05-02T06:50:51Z Abstract A perturbation method is used to analyse the stability of a thin till layer overlain by a deep ice layer. Ice is modelled as a linearly viscous fluid, while the till viscosity has power-law dependence on stress and effective pressure. A linearized set of equations yields descriptions of the coupling of the ice flow with the sediment flow and reveals parameter ranges where the till-perturbation amplitude can grow. This sheet-flow instability is an essential part of any theory of drumlin formation and shows that viscous models of till have the ability to explain typical deforming-bed features. This is of great significance for large-scale ice-sheet modelling. Article in Journal/Newspaper Ice Sheet Journal of Glaciology Cambridge University Press Journal of Glaciology 44 147 285 292
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract A perturbation method is used to analyse the stability of a thin till layer overlain by a deep ice layer. Ice is modelled as a linearly viscous fluid, while the till viscosity has power-law dependence on stress and effective pressure. A linearized set of equations yields descriptions of the coupling of the ice flow with the sediment flow and reveals parameter ranges where the till-perturbation amplitude can grow. This sheet-flow instability is an essential part of any theory of drumlin formation and shows that viscous models of till have the ability to explain typical deforming-bed features. This is of great significance for large-scale ice-sheet modelling.
format Article in Journal/Newspaper
author Hindmarsh, Richard C. A.
spellingShingle Hindmarsh, Richard C. A.
The stability of a viscous till sheet coupled with ice flow, considered at wavelengths less than the ice thickness
author_facet Hindmarsh, Richard C. A.
author_sort Hindmarsh, Richard C. A.
title The stability of a viscous till sheet coupled with ice flow, considered at wavelengths less than the ice thickness
title_short The stability of a viscous till sheet coupled with ice flow, considered at wavelengths less than the ice thickness
title_full The stability of a viscous till sheet coupled with ice flow, considered at wavelengths less than the ice thickness
title_fullStr The stability of a viscous till sheet coupled with ice flow, considered at wavelengths less than the ice thickness
title_full_unstemmed The stability of a viscous till sheet coupled with ice flow, considered at wavelengths less than the ice thickness
title_sort stability of a viscous till sheet coupled with ice flow, considered at wavelengths less than the ice thickness
publisher Cambridge University Press (CUP)
publishDate 1998
url http://dx.doi.org/10.1017/s0022143000002628
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000002628
genre Ice Sheet
Journal of Glaciology
genre_facet Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology
volume 44, issue 147, page 285-292
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000002628
container_title Journal of Glaciology
container_volume 44
container_issue 147
container_start_page 285
op_container_end_page 292
_version_ 1799481801735929856