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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Published in:Advances in Acoustics and Vibration
Main Author: Usama Kadri
Format: Article in Journal/Newspaper
Language:English
Published: Advances in Acoustics and Vibration 2016
Subjects:
Online Access:https://doi.org/10.1155/2016/8076108
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spelling fthindawi:oai:hindawi.com:10.1155/2016/8076108 2023-05-15T14:40:45+02:00 Generation of Hydroacoustic Waves by an Oscillating Ice Block in Arctic Zones Usama Kadri 2016 https://doi.org/10.1155/2016/8076108 en eng Advances in Acoustics and Vibration https://doi.org/10.1155/2016/8076108 Copyright © 2016 Usama Kadri. Research Article 2016 fthindawi https://doi.org/10.1155/2016/8076108 2019-05-26T06:48:54Z 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 Hindawi Publishing Corporation Arctic Advances in Acoustics and Vibration 2016 1 7
institution Open Polar
collection Hindawi Publishing Corporation
op_collection_id fthindawi
language English
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
author Usama Kadri
spellingShingle Usama Kadri
Generation of Hydroacoustic Waves by an Oscillating Ice Block in Arctic Zones
author_facet Usama Kadri
author_sort Usama Kadri
title 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_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_sort generation of hydroacoustic waves by an oscillating ice block in arctic zones
publisher Advances in Acoustics and Vibration
publishDate 2016
url https://doi.org/10.1155/2016/8076108
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_relation https://doi.org/10.1155/2016/8076108
op_rights Copyright © 2016 Usama Kadri.
op_doi https://doi.org/10.1155/2016/8076108
container_title Advances in Acoustics and Vibration
container_volume 2016
container_start_page 1
op_container_end_page 7
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