The Natural Oscillations of an Ice-Covered Channel
Abstract The natural modes of oscillation of an infinitely long, ice covered channel are considered, using the hydrostatic approximation, and assuming the ice to behave elastically. The dispersion relation, mode shape, and associated force on the channel wall are found for the lowest three modes. Sp...
| Published in: | Journal of Glaciology |
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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Cambridge University Press (CUP)
1984
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| Online Access: | http://dx.doi.org/10.1017/s0022143000006158 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006158 |
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crcambridgeupr:10.1017/s0022143000006158 |
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openpolar |
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crcambridgeupr:10.1017/s0022143000006158 2023-06-11T04:13:25+02:00 The Natural Oscillations of an Ice-Covered Channel Green, Theodore 1984 http://dx.doi.org/10.1017/s0022143000006158 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006158 en eng Cambridge University Press (CUP) Journal of Glaciology volume 30, issue 106, page 313-320 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1984 crcambridgeupr https://doi.org/10.1017/s0022143000006158 2023-05-01T18:22:00Z Abstract The natural modes of oscillation of an infinitely long, ice covered channel are considered, using the hydrostatic approximation, and assuming the ice to behave elastically. The dispersion relation, mode shape, and associated force on the channel wall are found for the lowest three modes. Special attention is paid to the limitations associated with the hydrostatic and elastic approximations. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press (via Crossref) Journal of Glaciology 30 106 313 320 |
| institution |
Open Polar |
| collection |
Cambridge University Press (via Crossref) |
| op_collection_id |
crcambridgeupr |
| language |
English |
| topic |
Earth-Surface Processes |
| spellingShingle |
Earth-Surface Processes Green, Theodore The Natural Oscillations of an Ice-Covered Channel |
| topic_facet |
Earth-Surface Processes |
| description |
Abstract The natural modes of oscillation of an infinitely long, ice covered channel are considered, using the hydrostatic approximation, and assuming the ice to behave elastically. The dispersion relation, mode shape, and associated force on the channel wall are found for the lowest three modes. Special attention is paid to the limitations associated with the hydrostatic and elastic approximations. |
| format |
Article in Journal/Newspaper |
| author |
Green, Theodore |
| author_facet |
Green, Theodore |
| author_sort |
Green, Theodore |
| title |
The Natural Oscillations of an Ice-Covered Channel |
| title_short |
The Natural Oscillations of an Ice-Covered Channel |
| title_full |
The Natural Oscillations of an Ice-Covered Channel |
| title_fullStr |
The Natural Oscillations of an Ice-Covered Channel |
| title_full_unstemmed |
The Natural Oscillations of an Ice-Covered Channel |
| title_sort |
natural oscillations of an ice-covered channel |
| publisher |
Cambridge University Press (CUP) |
| publishDate |
1984 |
| url |
http://dx.doi.org/10.1017/s0022143000006158 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006158 |
| genre |
Journal of Glaciology |
| genre_facet |
Journal of Glaciology |
| op_source |
Journal of Glaciology volume 30, issue 106, page 313-320 ISSN 0022-1430 1727-5652 |
| op_doi |
https://doi.org/10.1017/s0022143000006158 |
| container_title |
Journal of Glaciology |
| container_volume |
30 |
| container_issue |
106 |
| container_start_page |
313 |
| op_container_end_page |
320 |
| _version_ |
1768390452917043200 |