Equilibrium Profile of Ice Caps

Abstract Nye’s theory of the equilibrium profile of two-dimensional ice caps is modified to include longitudinal stress and creep rate effects. A more generalized law for the sliding velocity of a glacier over its bed is introduced into the analysis in order to permit the inclusion of these addition...

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Published in:Journal of Glaciology
Main Author: Weertman, J.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1961
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000017366
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000017366
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spelling crcambridgeupr:10.1017/s0022143000017366 2024-03-03T08:38:17+00:00 Equilibrium Profile of Ice Caps Weertman, J. 1961 http://dx.doi.org/10.1017/s0022143000017366 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000017366 en eng Cambridge University Press (CUP) Journal of Glaciology volume 3, issue 30, page 953-964 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1961 crcambridgeupr https://doi.org/10.1017/s0022143000017366 2024-02-08T08:37:11Z Abstract Nye’s theory of the equilibrium profile of two-dimensional ice caps is modified to include longitudinal stress and creep rate effects. A more generalized law for the sliding velocity of a glacier over its bed is introduced into the analysis in order to permit the inclusion of these additional complications. It is found that in the case of small ice caps (of the order of 30 km. in width), it is important to include the longitudinal stress. A somewhat “flatter” profile than that calculated by Nye is obtained. For ice sheets of the dimensions of the Greenland or Antarctic Ice Sheets, the additional stress causes essentially no modification in Nye’s theory. Nye’s theory also has been extended to include an isostatic sinking under the weight of the ice of the bedrock below an ice cap. Article in Journal/Newspaper Antarc* Antarctic glacier Greenland Ice cap Journal of Glaciology Cambridge University Press Antarctic Greenland Journal of Glaciology 3 30 953 964
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Weertman, J.
Equilibrium Profile of Ice Caps
topic_facet Earth-Surface Processes
description Abstract Nye’s theory of the equilibrium profile of two-dimensional ice caps is modified to include longitudinal stress and creep rate effects. A more generalized law for the sliding velocity of a glacier over its bed is introduced into the analysis in order to permit the inclusion of these additional complications. It is found that in the case of small ice caps (of the order of 30 km. in width), it is important to include the longitudinal stress. A somewhat “flatter” profile than that calculated by Nye is obtained. For ice sheets of the dimensions of the Greenland or Antarctic Ice Sheets, the additional stress causes essentially no modification in Nye’s theory. Nye’s theory also has been extended to include an isostatic sinking under the weight of the ice of the bedrock below an ice cap.
format Article in Journal/Newspaper
author Weertman, J.
author_facet Weertman, J.
author_sort Weertman, J.
title Equilibrium Profile of Ice Caps
title_short Equilibrium Profile of Ice Caps
title_full Equilibrium Profile of Ice Caps
title_fullStr Equilibrium Profile of Ice Caps
title_full_unstemmed Equilibrium Profile of Ice Caps
title_sort equilibrium profile of ice caps
publisher Cambridge University Press (CUP)
publishDate 1961
url http://dx.doi.org/10.1017/s0022143000017366
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000017366
geographic Antarctic
Greenland
geographic_facet Antarctic
Greenland
genre Antarc*
Antarctic
glacier
Greenland
Ice cap
Journal of Glaciology
genre_facet Antarc*
Antarctic
glacier
Greenland
Ice cap
Journal of Glaciology
op_source Journal of Glaciology
volume 3, issue 30, page 953-964
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000017366
container_title Journal of Glaciology
container_volume 3
container_issue 30
container_start_page 953
op_container_end_page 964
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