Rheology of Glacier Ice
A new method for calculating the stress field in bounded ice shelves is used to compare strain rate and deviatoric stress on the Ross Ice Shelf, Antarctica. The analysis shows that strain rate (per second) increases as the third power of deviatoric stress (in newtons per square meter), with a consta...
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American Association for the Advancement of Science (AAAS)
1985
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Online Access: | http://dx.doi.org/10.1126/science.227.4692.1335 https://www.science.org/doi/pdf/10.1126/science.227.4692.1335 |
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craaas:10.1126/science.227.4692.1335 2024-06-23T07:47:19+00:00 Rheology of Glacier Ice Jezek, Kenneth C. Alley, Richard B. Thomas, Robert H. 1985 http://dx.doi.org/10.1126/science.227.4692.1335 https://www.science.org/doi/pdf/10.1126/science.227.4692.1335 en eng American Association for the Advancement of Science (AAAS) Science volume 227, issue 4692, page 1335-1337 ISSN 0036-8075 1095-9203 journal-article 1985 craaas https://doi.org/10.1126/science.227.4692.1335 2024-06-06T04:01:26Z A new method for calculating the stress field in bounded ice shelves is used to compare strain rate and deviatoric stress on the Ross Ice Shelf, Antarctica. The analysis shows that strain rate (per second) increases as the third power of deviatoric stress (in newtons per square meter), with a constant of proportionality equal to 2.3 x 10 -25 . Article in Journal/Newspaper Antarc* Antarctica Ice Shelf Ice Shelves Ross Ice Shelf AAAS Resource Center (American Association for the Advancement of Science) Ross Ice Shelf Science 227 4692 1335 1337 |
institution |
Open Polar |
collection |
AAAS Resource Center (American Association for the Advancement of Science) |
op_collection_id |
craaas |
language |
English |
description |
A new method for calculating the stress field in bounded ice shelves is used to compare strain rate and deviatoric stress on the Ross Ice Shelf, Antarctica. The analysis shows that strain rate (per second) increases as the third power of deviatoric stress (in newtons per square meter), with a constant of proportionality equal to 2.3 x 10 -25 . |
format |
Article in Journal/Newspaper |
author |
Jezek, Kenneth C. Alley, Richard B. Thomas, Robert H. |
spellingShingle |
Jezek, Kenneth C. Alley, Richard B. Thomas, Robert H. Rheology of Glacier Ice |
author_facet |
Jezek, Kenneth C. Alley, Richard B. Thomas, Robert H. |
author_sort |
Jezek, Kenneth C. |
title |
Rheology of Glacier Ice |
title_short |
Rheology of Glacier Ice |
title_full |
Rheology of Glacier Ice |
title_fullStr |
Rheology of Glacier Ice |
title_full_unstemmed |
Rheology of Glacier Ice |
title_sort |
rheology of glacier ice |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
1985 |
url |
http://dx.doi.org/10.1126/science.227.4692.1335 https://www.science.org/doi/pdf/10.1126/science.227.4692.1335 |
geographic |
Ross Ice Shelf |
geographic_facet |
Ross Ice Shelf |
genre |
Antarc* Antarctica Ice Shelf Ice Shelves Ross Ice Shelf |
genre_facet |
Antarc* Antarctica Ice Shelf Ice Shelves Ross Ice Shelf |
op_source |
Science volume 227, issue 4692, page 1335-1337 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.227.4692.1335 |
container_title |
Science |
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227 |
container_issue |
4692 |
container_start_page |
1335 |
op_container_end_page |
1337 |
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1802651415611441152 |