Reflection and transmission of ocean wave spectra by a band of randomly distributed ice floes
A new ocean wave/sea-ice interaction model is proposed that simulates how a directional wave spectrum evolves as it travels through an arbitrary finite array of circular ice floes, where wave/ice dynamics are entirely governed by wave-scattering effects. The model is applied to characterize the wave...
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Language: | English |
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International Glaciological Society
2015
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Online Access: | http://hdl.handle.net/2440/96371 https://doi.org/10.3189/2015AoG69A556 |
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ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/96371 2023-12-24T10:08:24+01:00 Reflection and transmission of ocean wave spectra by a band of randomly distributed ice floes Montiel, F. Squire, V. Bennetts, L. 2015 http://hdl.handle.net/2440/96371 https://doi.org/10.3189/2015AoG69A556 en eng International Glaciological Society http://purl.org/au-research/grants/arc/DE130101571 Annals of Glaciology, 2015; 56(69):315-322 0260-3055 1727-5644 http://hdl.handle.net/2440/96371 doi:10.3189/2015AoG69A556 Bennetts, L. [0000-0001-9386-7882] Copyright status unknown http://dx.doi.org/10.3189/2015aog69a556 Journal article 2015 ftunivadelaidedl https://doi.org/10.3189/2015AoG69A55610.3189/2015aog69a556 2023-11-27T23:18:44Z A new ocean wave/sea-ice interaction model is proposed that simulates how a directional wave spectrum evolves as it travels through an arbitrary finite array of circular ice floes, where wave/ice dynamics are entirely governed by wave-scattering effects. The model is applied to characterize the wave reflection and transmission properties of a strip of ice floes, such as an ice edge band. A method is devised to extract the reflected and transmitted directional wave spectra produced by the array. The method builds upon an integral mapping from polar to Cartesian coordinates of the scattered wave components. Sensitivity tests are conducted for a row of floes randomly perturbed from a regular arrangement. Results for random arrays are generated using ensemble averaging. A realistic ice edge band is then reconstructed from field experiment data. Simulations show good qualitative agreement with the data in terms of transmitted wave energy and directional spreading. In particular, it is observed that short waves become isotropic quickly after penetrating the ice field. Fabien Montiel, Vernon A. Squire, Luke G. Bennetts Article in Journal/Newspaper Annals of Glaciology Sea ice The University of Adelaide: Digital Library Luke ENVELOPE(-94.855,-94.855,56.296,56.296) Annals of Glaciology 56 69 315 322 |
institution |
Open Polar |
collection |
The University of Adelaide: Digital Library |
op_collection_id |
ftunivadelaidedl |
language |
English |
description |
A new ocean wave/sea-ice interaction model is proposed that simulates how a directional wave spectrum evolves as it travels through an arbitrary finite array of circular ice floes, where wave/ice dynamics are entirely governed by wave-scattering effects. The model is applied to characterize the wave reflection and transmission properties of a strip of ice floes, such as an ice edge band. A method is devised to extract the reflected and transmitted directional wave spectra produced by the array. The method builds upon an integral mapping from polar to Cartesian coordinates of the scattered wave components. Sensitivity tests are conducted for a row of floes randomly perturbed from a regular arrangement. Results for random arrays are generated using ensemble averaging. A realistic ice edge band is then reconstructed from field experiment data. Simulations show good qualitative agreement with the data in terms of transmitted wave energy and directional spreading. In particular, it is observed that short waves become isotropic quickly after penetrating the ice field. Fabien Montiel, Vernon A. Squire, Luke G. Bennetts |
format |
Article in Journal/Newspaper |
author |
Montiel, F. Squire, V. Bennetts, L. |
spellingShingle |
Montiel, F. Squire, V. Bennetts, L. Reflection and transmission of ocean wave spectra by a band of randomly distributed ice floes |
author_facet |
Montiel, F. Squire, V. Bennetts, L. |
author_sort |
Montiel, F. |
title |
Reflection and transmission of ocean wave spectra by a band of randomly distributed ice floes |
title_short |
Reflection and transmission of ocean wave spectra by a band of randomly distributed ice floes |
title_full |
Reflection and transmission of ocean wave spectra by a band of randomly distributed ice floes |
title_fullStr |
Reflection and transmission of ocean wave spectra by a band of randomly distributed ice floes |
title_full_unstemmed |
Reflection and transmission of ocean wave spectra by a band of randomly distributed ice floes |
title_sort |
reflection and transmission of ocean wave spectra by a band of randomly distributed ice floes |
publisher |
International Glaciological Society |
publishDate |
2015 |
url |
http://hdl.handle.net/2440/96371 https://doi.org/10.3189/2015AoG69A556 |
long_lat |
ENVELOPE(-94.855,-94.855,56.296,56.296) |
geographic |
Luke |
geographic_facet |
Luke |
genre |
Annals of Glaciology Sea ice |
genre_facet |
Annals of Glaciology Sea ice |
op_source |
http://dx.doi.org/10.3189/2015aog69a556 |
op_relation |
http://purl.org/au-research/grants/arc/DE130101571 Annals of Glaciology, 2015; 56(69):315-322 0260-3055 1727-5644 http://hdl.handle.net/2440/96371 doi:10.3189/2015AoG69A556 Bennetts, L. [0000-0001-9386-7882] |
op_rights |
Copyright status unknown |
op_doi |
https://doi.org/10.3189/2015AoG69A55610.3189/2015aog69a556 |
container_title |
Annals of Glaciology |
container_volume |
56 |
container_issue |
69 |
container_start_page |
315 |
op_container_end_page |
322 |
_version_ |
1786199048520204288 |