Gravitational Stresses in Floating Ice Sheets

Abstract This note is addressed to the determination of the in-plane components of stress in floating ice sheets due to gravity and the hydrostatic pressure in the water. The distribution and magnitude of these stresses are of interest with regard to crack propagation in sea ice. Two cases are consi...

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Published in:Journal of Glaciology
Main Authors: Evans, R.J., Parmerter, R. Reid
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1979
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000014179
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014179
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spelling crcambridgeupr:10.1017/s0022143000014179 2024-03-03T08:36:55+00:00 Gravitational Stresses in Floating Ice Sheets Evans, R.J. Parmerter, R. Reid 1979 http://dx.doi.org/10.1017/s0022143000014179 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014179 en eng Cambridge University Press (CUP) Journal of Glaciology volume 22, issue 86, page 182-185 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1979 crcambridgeupr https://doi.org/10.1017/s0022143000014179 2024-02-08T08:39:08Z Abstract This note is addressed to the determination of the in-plane components of stress in floating ice sheets due to gravity and the hydrostatic pressure in the water. The distribution and magnitude of these stresses are of interest with regard to crack propagation in sea ice. Two cases are considered. In the first, the ice sheet is formed on land by accretion at the top surface and then introduced into the water, such as happens in the Antarctic. In the second, the ice is formed in the water by accretion on the bottom, which is the usual situation in the Arctic pack ice. Article in Journal/Newspaper Antarc* Antarctic Arctic Ice Sheet Journal of Glaciology Sea ice Cambridge University Press Arctic Antarctic The Antarctic Journal of Glaciology 22 86 182 185
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Evans, R.J.
Parmerter, R. Reid
Gravitational Stresses in Floating Ice Sheets
topic_facet Earth-Surface Processes
description Abstract This note is addressed to the determination of the in-plane components of stress in floating ice sheets due to gravity and the hydrostatic pressure in the water. The distribution and magnitude of these stresses are of interest with regard to crack propagation in sea ice. Two cases are considered. In the first, the ice sheet is formed on land by accretion at the top surface and then introduced into the water, such as happens in the Antarctic. In the second, the ice is formed in the water by accretion on the bottom, which is the usual situation in the Arctic pack ice.
format Article in Journal/Newspaper
author Evans, R.J.
Parmerter, R. Reid
author_facet Evans, R.J.
Parmerter, R. Reid
author_sort Evans, R.J.
title Gravitational Stresses in Floating Ice Sheets
title_short Gravitational Stresses in Floating Ice Sheets
title_full Gravitational Stresses in Floating Ice Sheets
title_fullStr Gravitational Stresses in Floating Ice Sheets
title_full_unstemmed Gravitational Stresses in Floating Ice Sheets
title_sort gravitational stresses in floating ice sheets
publisher Cambridge University Press (CUP)
publishDate 1979
url http://dx.doi.org/10.1017/s0022143000014179
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014179
geographic Arctic
Antarctic
The Antarctic
geographic_facet Arctic
Antarctic
The Antarctic
genre Antarc*
Antarctic
Arctic
Ice Sheet
Journal of Glaciology
Sea ice
genre_facet Antarc*
Antarctic
Arctic
Ice Sheet
Journal of Glaciology
Sea ice
op_source Journal of Glaciology
volume 22, issue 86, page 182-185
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000014179
container_title Journal of Glaciology
container_volume 22
container_issue 86
container_start_page 182
op_container_end_page 185
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