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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Published in:Journal of Glaciology
Main Author: Thomas, R.H.
Format: Article in Journal/Newspaper
Language:unknown
Published: International Glaciological Society 1973
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/526106/
https://doi.org/10.3189/S0022143000022693
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spelling 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
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id 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
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