The creep of ice shelves theory
Budd’s expressions for strain-rate gradient along the centre line of a bounded ice shelf are shown to be applicable only to ice shelves with almost constant thickness and very small longitudinal strain-rates. A general expression is derived for creep in an ice shelf where the sole restriction is tha...
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International Glaciological Society
1973
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Online Access: | http://nora.nerc.ac.uk/id/eprint/526106/ https://doi.org/10.3189/S0022143000022693 |
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ftnerc:oai:nora.nerc.ac.uk:526106 2023-05-15T16:41:43+02:00 The creep of ice shelves theory Thomas, R.H. 1973 http://nora.nerc.ac.uk/id/eprint/526106/ https://doi.org/10.3189/S0022143000022693 unknown International Glaciological Society Thomas, R.H. 1973 The creep of ice shelves theory. Journal of Glaciology, 12 (64). 45-53. https://doi.org/10.3189/S0022143000022693 <https://doi.org/10.3189/S0022143000022693> Publication - Article PeerReviewed 1973 ftnerc https://doi.org/10.3189/S0022143000022693 2023-02-04T19:49:47Z Budd’s expressions for strain-rate gradient along the centre line of a bounded ice shelf are shown to be applicable only to ice shelves with almost constant thickness and very small longitudinal strain-rates. A general expression is derived for creep in an ice shelf where the sole restriction is that of zero shear stresses in vertical planes. This is applied to the two special cases: (1)movement of an ice shelf restricted in at least one direction by sea-water pressure only; (2)movement of an ice shelf flowing between roughly parallel sides. Article in Journal/Newspaper Ice Shelf Ice Shelves Journal of Glaciology Natural Environment Research Council: NERC Open Research Archive Journal of Glaciology 12 64 45 53 |
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Open Polar |
collection |
Natural Environment Research Council: NERC Open Research Archive |
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ftnerc |
language |
unknown |
description |
Budd’s expressions for strain-rate gradient along the centre line of a bounded ice shelf are shown to be applicable only to ice shelves with almost constant thickness and very small longitudinal strain-rates. A general expression is derived for creep in an ice shelf where the sole restriction is that of zero shear stresses in vertical planes. This is applied to the two special cases: (1)movement of an ice shelf restricted in at least one direction by sea-water pressure only; (2)movement of an ice shelf flowing between roughly parallel sides. |
format |
Article in Journal/Newspaper |
author |
Thomas, R.H. |
spellingShingle |
Thomas, R.H. The creep of ice shelves theory |
author_facet |
Thomas, R.H. |
author_sort |
Thomas, R.H. |
title |
The creep of ice shelves theory |
title_short |
The creep of ice shelves theory |
title_full |
The creep of ice shelves theory |
title_fullStr |
The creep of ice shelves theory |
title_full_unstemmed |
The creep of ice shelves theory |
title_sort |
creep of ice shelves theory |
publisher |
International Glaciological Society |
publishDate |
1973 |
url |
http://nora.nerc.ac.uk/id/eprint/526106/ https://doi.org/10.3189/S0022143000022693 |
genre |
Ice Shelf Ice Shelves Journal of Glaciology |
genre_facet |
Ice Shelf Ice Shelves Journal of Glaciology |
op_relation |
Thomas, R.H. 1973 The creep of ice shelves theory. Journal of Glaciology, 12 (64). 45-53. https://doi.org/10.3189/S0022143000022693 <https://doi.org/10.3189/S0022143000022693> |
op_doi |
https://doi.org/10.3189/S0022143000022693 |
container_title |
Journal of Glaciology |
container_volume |
12 |
container_issue |
64 |
container_start_page |
45 |
op_container_end_page |
53 |
_version_ |
1766032188658155520 |