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...
Published in: | Journal of Glaciology |
---|---|
Main Author: | |
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 |