How waves break up inshore fast ice
Abstract Vertical accelerometers deployed on fast ice in Raudfjorden, Svalbard in early summer 1983 recorded characteristics of ice-coupled waves at the ice edge and during their passage under die ice sheet. Subsequent analysis indicated an unexpected increase in amplitude of waves of all periods so...
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Cambridge University Press (CUP)
1984
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Online Access: | http://dx.doi.org/10.1017/s0032247400005404 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400005404 |
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crcambridgeupr:10.1017/s0032247400005404 2024-09-15T18:12:21+00:00 How waves break up inshore fast ice Squire, Vernon A. 1984 http://dx.doi.org/10.1017/s0032247400005404 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400005404 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Polar Record volume 22, issue 138, page 281-285 ISSN 0032-2474 1475-3057 journal-article 1984 crcambridgeupr https://doi.org/10.1017/s0032247400005404 2024-08-07T04:04:03Z Abstract Vertical accelerometers deployed on fast ice in Raudfjorden, Svalbard in early summer 1983 recorded characteristics of ice-coupled waves at the ice edge and during their passage under die ice sheet. Subsequent analysis indicated an unexpected increase in amplitude of waves of all periods some 20 to 30 m in from die ice edge. This is associated with a pair of heavily-damped waves, which become especially relevant at or beyond some critical angle and decay rapidly with distance from the edge; their coalescence may account for the increase in wave amplitude, and explain why ice tends to break out in strips parallel to the ice edge. Article in Journal/Newspaper Ice Sheet Polar Record Svalbard Cambridge University Press Polar Record 22 138 281 285 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
Abstract Vertical accelerometers deployed on fast ice in Raudfjorden, Svalbard in early summer 1983 recorded characteristics of ice-coupled waves at the ice edge and during their passage under die ice sheet. Subsequent analysis indicated an unexpected increase in amplitude of waves of all periods some 20 to 30 m in from die ice edge. This is associated with a pair of heavily-damped waves, which become especially relevant at or beyond some critical angle and decay rapidly with distance from the edge; their coalescence may account for the increase in wave amplitude, and explain why ice tends to break out in strips parallel to the ice edge. |
format |
Article in Journal/Newspaper |
author |
Squire, Vernon A. |
spellingShingle |
Squire, Vernon A. How waves break up inshore fast ice |
author_facet |
Squire, Vernon A. |
author_sort |
Squire, Vernon A. |
title |
How waves break up inshore fast ice |
title_short |
How waves break up inshore fast ice |
title_full |
How waves break up inshore fast ice |
title_fullStr |
How waves break up inshore fast ice |
title_full_unstemmed |
How waves break up inshore fast ice |
title_sort |
how waves break up inshore fast ice |
publisher |
Cambridge University Press (CUP) |
publishDate |
1984 |
url |
http://dx.doi.org/10.1017/s0032247400005404 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400005404 |
genre |
Ice Sheet Polar Record Svalbard |
genre_facet |
Ice Sheet Polar Record Svalbard |
op_source |
Polar Record volume 22, issue 138, page 281-285 ISSN 0032-2474 1475-3057 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0032247400005404 |
container_title |
Polar Record |
container_volume |
22 |
container_issue |
138 |
container_start_page |
281 |
op_container_end_page |
285 |
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1810449931480072192 |