A Kinematic Wave Model of Glacier Surges

Abstract The existing theory of kinematic waves on glaciers does not account for self-induced instability of the flow, or for surges which are not the result of external disturbances. Surges do however have much in common with kinematic waves. Unstable behaviour of glaciers can be explained by a str...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Palmer, Andrew C.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1972
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000022504
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000022504
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spelling crcambridgeupr:10.1017/s0022143000022504 2024-03-03T08:46:01+00:00 A Kinematic Wave Model of Glacier Surges Palmer, Andrew C. 1972 http://dx.doi.org/10.1017/s0022143000022504 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000022504 en eng Cambridge University Press (CUP) Journal of Glaciology volume 11, issue 61, page 65-72 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1972 crcambridgeupr https://doi.org/10.1017/s0022143000022504 2024-02-08T08:32:56Z Abstract The existing theory of kinematic waves on glaciers does not account for self-induced instability of the flow, or for surges which are not the result of external disturbances. Surges do however have much in common with kinematic waves. Unstable behaviour of glaciers can be explained by a straightforward modification of kinematic wave theory. In this modification the relation between the ice flow and the ice depth is not the same when the ice is accelerating as when it is slowing down. A similar effect has previously been shown to explain observed instabilities in the flow of highway traffic, a phenomenon which is otherwise adequately described by a simple kinematic wave theory. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 11 61 65 72
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Palmer, Andrew C.
A Kinematic Wave Model of Glacier Surges
topic_facet Earth-Surface Processes
description Abstract The existing theory of kinematic waves on glaciers does not account for self-induced instability of the flow, or for surges which are not the result of external disturbances. Surges do however have much in common with kinematic waves. Unstable behaviour of glaciers can be explained by a straightforward modification of kinematic wave theory. In this modification the relation between the ice flow and the ice depth is not the same when the ice is accelerating as when it is slowing down. A similar effect has previously been shown to explain observed instabilities in the flow of highway traffic, a phenomenon which is otherwise adequately described by a simple kinematic wave theory.
format Article in Journal/Newspaper
author Palmer, Andrew C.
author_facet Palmer, Andrew C.
author_sort Palmer, Andrew C.
title A Kinematic Wave Model of Glacier Surges
title_short A Kinematic Wave Model of Glacier Surges
title_full A Kinematic Wave Model of Glacier Surges
title_fullStr A Kinematic Wave Model of Glacier Surges
title_full_unstemmed A Kinematic Wave Model of Glacier Surges
title_sort kinematic wave model of glacier surges
publisher Cambridge University Press (CUP)
publishDate 1972
url http://dx.doi.org/10.1017/s0022143000022504
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000022504
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 11, issue 61, page 65-72
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000022504
container_title Journal of Glaciology
container_volume 11
container_issue 61
container_start_page 65
op_container_end_page 72
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