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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Published in:Science
Main Authors: Jezek, Kenneth C., Alley, Richard B., Thomas, Robert H.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1985
Subjects:
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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spelling 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
container_volume 227
container_issue 4692
container_start_page 1335
op_container_end_page 1337
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