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...

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Main Author: Kadri, Usama
Other Authors: Massachusetts Institute of Technology. Department of Mathematics
Format: Article
Language:English
Published: Hindawi Publishing Corporation 2016
Online Access:http://hdl.handle.net/1721.1/103895
https://orcid.org/0000-0002-5441-1812
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author Kadri, Usama
author2 Massachusetts Institute of Technology. Department of Mathematics
author_facet Massachusetts Institute of Technology. Department of Mathematics
Kadri, Usama
author_sort Kadri, Usama
collection MIT
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.
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spelling mit-1721.1/1038952022-09-30T07:48:34Z Generation of Hydroacoustic Waves by an Oscillating Ice Block in Arctic Zones Kadri, Usama Massachusetts Institute of Technology. Department of Mathematics Kadri, Usama 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. 2016-08-11T15:25:34Z 2016-08-11T15:25:34Z 2016-07 2016-06 2016-08-03T07:47:57Z Article http://purl.org/eprint/type/JournalArticle 1687-6261 1687-627X http://hdl.handle.net/1721.1/103895 Kadri, Usama. "Generation of Hydroacoustic Waves by an Oscillating Ice Block in Arctic Zones." Advances in Acoustics and Vibration 2016 (2016), Article ID 8076108, pp. 1-7. https://orcid.org/0000-0002-5441-1812 en http://dx.doi.org/10.1155/2016/8076108 Advances in Acoustics and Vibration 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. application/pdf Hindawi Publishing Corporation Hindawi Publishing Corporation
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
https://orcid.org/0000-0002-5441-1812
work_keys_str_mv AT kadriusama generationofhydroacousticwavesbyanoscillatingiceblockinarcticzones