Generation of Hydroacoustic Waves by an Oscillating Ice Block in Arctic Zones
The time harmonic problem of propagating hydroacoustic waves generated in the ocean by a vertically oscillating ice block in arctic zones is discussed. The generated acoustic modes can result in orbital displacements of fluid parcels sufficiently high that may contribute to deep ocean currents and c...
Published in: | Advances in Acoustics and Vibration |
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Main Author: | |
Other Authors: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Hindawi Publishing Corporation
2016
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Subjects: | |
Online Access: | http://hdl.handle.net/1721.1/103895 |
_version_ | 1829947222909779968 |
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author | Kadri, Usama |
author2 | Massachusetts Institute of Technology. Department of Mathematics Kadri, Usama |
author_facet | Kadri, Usama |
author_sort | Kadri, Usama |
collection | DSpace@MIT (Massachusetts Institute of Technology) |
container_start_page | 1 |
container_title | Advances in Acoustics and Vibration |
container_volume | 2016 |
description | The time harmonic problem of propagating hydroacoustic waves generated in the ocean by a vertically oscillating ice block in arctic zones is discussed. The generated acoustic modes can result in orbital displacements of fluid parcels sufficiently high that may contribute to deep ocean currents and circulation. This mechanism adds to current efforts for explaining ocean circulation from a snowball earth Neoproterozoic Era to greenhouse earth arctic conditions and raises a challenge as the extent of ice blocks shrinks towards an ice-free sea. Surprisingly, unlike the free-surface setting, here it is found that the higher acoustic modes exhibit a larger contribution. |
format | Article in Journal/Newspaper |
genre | Arctic |
genre_facet | Arctic |
geographic | Arctic |
geographic_facet | Arctic |
id | ftmit:oai:dspace.mit.edu:1721.1/103895 |
institution | Open Polar |
language | English |
op_collection_id | ftmit |
op_container_end_page | 7 |
op_doi | https://doi.org/10.1155/2016/8076108 |
op_relation | http://dx.doi.org/10.1155/2016/8076108 Advances in Acoustics and Vibration http://hdl.handle.net/1721.1/103895 |
op_rights | Creative Commons Attribution http://creativecommons.org/licenses/by/2.0 Copyright © 2016 Usama Kadri. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. |
op_source | Hindawi Publishing Corporation |
publishDate | 2016 |
publisher | Hindawi Publishing Corporation |
record_format | openpolar |
spelling | ftmit:oai:dspace.mit.edu:1721.1/103895 2025-04-20T14:30:42+00:00 Generation of Hydroacoustic Waves by an Oscillating Ice Block in Arctic Zones Kadri, Usama Massachusetts Institute of Technology. Department of Mathematics Kadri, Usama 2016-08-03T07:47:57Z application/pdf http://hdl.handle.net/1721.1/103895 en eng Hindawi Publishing Corporation http://dx.doi.org/10.1155/2016/8076108 Advances in Acoustics and Vibration http://hdl.handle.net/1721.1/103895 Creative Commons Attribution http://creativecommons.org/licenses/by/2.0 Copyright © 2016 Usama Kadri. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Hindawi Publishing Corporation Article http://purl.org/eprint/type/JournalArticle 2016 ftmit https://doi.org/10.1155/2016/8076108 2025-03-21T06:47:43Z The time harmonic problem of propagating hydroacoustic waves generated in the ocean by a vertically oscillating ice block in arctic zones is discussed. The generated acoustic modes can result in orbital displacements of fluid parcels sufficiently high that may contribute to deep ocean currents and circulation. This mechanism adds to current efforts for explaining ocean circulation from a snowball earth Neoproterozoic Era to greenhouse earth arctic conditions and raises a challenge as the extent of ice blocks shrinks towards an ice-free sea. Surprisingly, unlike the free-surface setting, here it is found that the higher acoustic modes exhibit a larger contribution. Article in Journal/Newspaper Arctic DSpace@MIT (Massachusetts Institute of Technology) Arctic Advances in Acoustics and Vibration 2016 1 7 |
spellingShingle | Kadri, Usama Generation of Hydroacoustic Waves by an Oscillating Ice Block in Arctic Zones |
title | Generation of Hydroacoustic Waves by an Oscillating Ice Block in Arctic Zones |
title_full | Generation of Hydroacoustic Waves by an Oscillating Ice Block in Arctic Zones |
title_fullStr | Generation of Hydroacoustic Waves by an Oscillating Ice Block in Arctic Zones |
title_full_unstemmed | Generation of Hydroacoustic Waves by an Oscillating Ice Block in Arctic Zones |
title_short | Generation of Hydroacoustic Waves by an Oscillating Ice Block in Arctic Zones |
title_sort | generation of hydroacoustic waves by an oscillating ice block in arctic zones |
url | http://hdl.handle.net/1721.1/103895 |