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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Cambridge University Press (CUP)
1979
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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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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 |
_version_ |
1792496383131910144 |