Experimental and theoretical models of wave-induced flexure of a sea ice floe
An experimental model is used to validate a theoretical model of a sea ice floe’s flexural motion, induced by ocean waves. A thin plastic plate models the ice floe in the experiments. Rigid and compliant plastics and two different thicknesses are tested. Regular incident waves are used, with wavelen...
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Language: | English |
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craippubl:10.1063/1.4916573 2024-09-15T18:34:42+00:00 Experimental and theoretical models of wave-induced flexure of a sea ice floe Meylan, M. H. Bennetts, L. G. Cavaliere, C. Alberello, A. Toffoli, A. Australian Antarctic Science Grant Program Office of Naval Research Plymouth University Australian Research Council 2015 http://dx.doi.org/10.1063/1.4916573 https://pubs.aip.org/aip/pof/article-pdf/doi/10.1063/1.4916573/16129779/041704_1_online.pdf en eng AIP Publishing Physics of Fluids volume 27, issue 4 ISSN 1070-6631 1089-7666 journal-article 2015 craippubl https://doi.org/10.1063/1.4916573 2024-08-01T04:04:00Z An experimental model is used to validate a theoretical model of a sea ice floe’s flexural motion, induced by ocean waves. A thin plastic plate models the ice floe in the experiments. Rigid and compliant plastics and two different thicknesses are tested. Regular incident waves are used, with wavelengths less than, equal to, and greater than the floe length, and steepnesses ranging from gently sloping to storm-like. Results show the models agree well, despite the overwash phenomenon occurring in the experiments, which the theoretical model neglects. Article in Journal/Newspaper Sea ice AIP Publishing Physics of Fluids 27 4 041704 |
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Open Polar |
collection |
AIP Publishing |
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craippubl |
language |
English |
description |
An experimental model is used to validate a theoretical model of a sea ice floe’s flexural motion, induced by ocean waves. A thin plastic plate models the ice floe in the experiments. Rigid and compliant plastics and two different thicknesses are tested. Regular incident waves are used, with wavelengths less than, equal to, and greater than the floe length, and steepnesses ranging from gently sloping to storm-like. Results show the models agree well, despite the overwash phenomenon occurring in the experiments, which the theoretical model neglects. |
author2 |
Australian Antarctic Science Grant Program Office of Naval Research Plymouth University Australian Research Council |
format |
Article in Journal/Newspaper |
author |
Meylan, M. H. Bennetts, L. G. Cavaliere, C. Alberello, A. Toffoli, A. |
spellingShingle |
Meylan, M. H. Bennetts, L. G. Cavaliere, C. Alberello, A. Toffoli, A. Experimental and theoretical models of wave-induced flexure of a sea ice floe |
author_facet |
Meylan, M. H. Bennetts, L. G. Cavaliere, C. Alberello, A. Toffoli, A. |
author_sort |
Meylan, M. H. |
title |
Experimental and theoretical models of wave-induced flexure of a sea ice floe |
title_short |
Experimental and theoretical models of wave-induced flexure of a sea ice floe |
title_full |
Experimental and theoretical models of wave-induced flexure of a sea ice floe |
title_fullStr |
Experimental and theoretical models of wave-induced flexure of a sea ice floe |
title_full_unstemmed |
Experimental and theoretical models of wave-induced flexure of a sea ice floe |
title_sort |
experimental and theoretical models of wave-induced flexure of a sea ice floe |
publisher |
AIP Publishing |
publishDate |
2015 |
url |
http://dx.doi.org/10.1063/1.4916573 https://pubs.aip.org/aip/pof/article-pdf/doi/10.1063/1.4916573/16129779/041704_1_online.pdf |
genre |
Sea ice |
genre_facet |
Sea ice |
op_source |
Physics of Fluids volume 27, issue 4 ISSN 1070-6631 1089-7666 |
op_doi |
https://doi.org/10.1063/1.4916573 |
container_title |
Physics of Fluids |
container_volume |
27 |
container_issue |
4 |
container_start_page |
041704 |
_version_ |
1810476645486690304 |