Dissipation Of Tidal Energy By Flexing Ice Shelves

Plastic deformation of ice shelves in the region along the grounding line where they bend with the tide can dissipate enough tidal energy to make them the most important single source contribution to tidal friction (Doake, 1978). Some of the effects are to slow the rotation of the Earth and to cause...

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Published in:Journal of Glaciology
Main Author: Doake, C. S. M.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1979
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000014970
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014970
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spelling crcambridgeupr:10.1017/s0022143000014970 2024-03-03T08:45:29+00:00 Dissipation Of Tidal Energy By Flexing Ice Shelves Doake, C. S. M. 1979 http://dx.doi.org/10.1017/s0022143000014970 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014970 en eng Cambridge University Press (CUP) Journal of Glaciology volume 24, issue 90, page 482 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1979 crcambridgeupr https://doi.org/10.1017/s0022143000014970 2024-02-08T08:42:50Z Plastic deformation of ice shelves in the region along the grounding line where they bend with the tide can dissipate enough tidal energy to make them the most important single source contribution to tidal friction (Doake, 1978). Some of the effects are to slow the rotation of the Earth and to cause the moon to retreat from the Earth. Article in Journal/Newspaper Ice Shelves Journal of Glaciology Cambridge University Press Journal of Glaciology 24 90 482
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Doake, C. S. M.
Dissipation Of Tidal Energy By Flexing Ice Shelves
topic_facet Earth-Surface Processes
description Plastic deformation of ice shelves in the region along the grounding line where they bend with the tide can dissipate enough tidal energy to make them the most important single source contribution to tidal friction (Doake, 1978). Some of the effects are to slow the rotation of the Earth and to cause the moon to retreat from the Earth.
format Article in Journal/Newspaper
author Doake, C. S. M.
author_facet Doake, C. S. M.
author_sort Doake, C. S. M.
title Dissipation Of Tidal Energy By Flexing Ice Shelves
title_short Dissipation Of Tidal Energy By Flexing Ice Shelves
title_full Dissipation Of Tidal Energy By Flexing Ice Shelves
title_fullStr Dissipation Of Tidal Energy By Flexing Ice Shelves
title_full_unstemmed Dissipation Of Tidal Energy By Flexing Ice Shelves
title_sort dissipation of tidal energy by flexing ice shelves
publisher Cambridge University Press (CUP)
publishDate 1979
url http://dx.doi.org/10.1017/s0022143000014970
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014970
genre Ice Shelves
Journal of Glaciology
genre_facet Ice Shelves
Journal of Glaciology
op_source Journal of Glaciology
volume 24, issue 90, page 482
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000014970
container_title Journal of Glaciology
container_volume 24
container_issue 90
container_start_page 482
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