Three-dimensional time-domain scattering of waves in the marginal ice zone

Three-dimensional scattering of ocean surface waves in the marginal ice zone (MIZ) is determined in the time domain. The solution is found using spectral analysis of the linear operator for the Boltzmann equation. The method to calculate the scattering kernel that arises in the Boltzmann model from...

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Main Authors: Meylan, M. H., Bennetts, L. G.
Other Authors: The University of Newcastle. Faculty of Science, School of Mathematical and Physical Sciences
Format: Article in Journal/Newspaper
Language:English
Published: Royal Society Publishing 2018
Subjects:
Online Access:http://hdl.handle.net/1959.13/1393615
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spelling ftunivnewcastnsw:uon:33563 2023-05-15T18:17:50+02:00 Three-dimensional time-domain scattering of waves in the marginal ice zone Meylan, M. H. Bennetts, L. G. The University of Newcastle. Faculty of Science, School of Mathematical and Physical Sciences 2018 http://hdl.handle.net/1959.13/1393615 eng eng Royal Society Publishing Royal Society of London. Philosophical Transactions A. Mathematical, Physical, and Engineering Sciences Vol. 376, Issue 2129, p. 1-19 10.1098/rsta.2017.0334 ­© 2018 The Authors. Published by the Royal Society under the terms of the Creative Commons Attribution License http://creativecommons.org/licenses/ by/4.0/, which permits unrestricted use, provided the original author and source are credited. CC-BY sea ice wave scattering marginal ice zone journal article 2018 ftunivnewcastnsw 2019-09-09T22:24:50Z Three-dimensional scattering of ocean surface waves in the marginal ice zone (MIZ) is determined in the time domain. The solution is found using spectral analysis of the linear operator for the Boltzmann equation. The method to calculate the scattering kernel that arises in the Boltzmann model from the single-floe solution is also presented along with new identities for the far-field scattering, which can be used to validate the single-floe solution. The spectrum of the operator is computed, and it is shown to have a universal structure under a special non-dimensionalization. This universal structure implies that under a scaling wave scattering in the MIZ has similar properties for a large range of ice types and wave periods. A scattering theory solution using fast Fourier transforms is given to find the solution for directional incident wave packets. A numerical solution method is also given using the split-step method and this is used to validate the spectral solution. Numerical calculations of the evolution of a typical wave field are presented. This article is part of the theme issue 'Modelling of sea-ice phenomena'. Article in Journal/Newspaper Sea ice NOVA: The University of Newcastle Research Online (Australia)
institution Open Polar
collection NOVA: The University of Newcastle Research Online (Australia)
op_collection_id ftunivnewcastnsw
language English
topic sea ice
wave scattering
marginal ice zone
spellingShingle sea ice
wave scattering
marginal ice zone
Meylan, M. H.
Bennetts, L. G.
Three-dimensional time-domain scattering of waves in the marginal ice zone
topic_facet sea ice
wave scattering
marginal ice zone
description Three-dimensional scattering of ocean surface waves in the marginal ice zone (MIZ) is determined in the time domain. The solution is found using spectral analysis of the linear operator for the Boltzmann equation. The method to calculate the scattering kernel that arises in the Boltzmann model from the single-floe solution is also presented along with new identities for the far-field scattering, which can be used to validate the single-floe solution. The spectrum of the operator is computed, and it is shown to have a universal structure under a special non-dimensionalization. This universal structure implies that under a scaling wave scattering in the MIZ has similar properties for a large range of ice types and wave periods. A scattering theory solution using fast Fourier transforms is given to find the solution for directional incident wave packets. A numerical solution method is also given using the split-step method and this is used to validate the spectral solution. Numerical calculations of the evolution of a typical wave field are presented. This article is part of the theme issue 'Modelling of sea-ice phenomena'.
author2 The University of Newcastle. Faculty of Science, School of Mathematical and Physical Sciences
format Article in Journal/Newspaper
author Meylan, M. H.
Bennetts, L. G.
author_facet Meylan, M. H.
Bennetts, L. G.
author_sort Meylan, M. H.
title Three-dimensional time-domain scattering of waves in the marginal ice zone
title_short Three-dimensional time-domain scattering of waves in the marginal ice zone
title_full Three-dimensional time-domain scattering of waves in the marginal ice zone
title_fullStr Three-dimensional time-domain scattering of waves in the marginal ice zone
title_full_unstemmed Three-dimensional time-domain scattering of waves in the marginal ice zone
title_sort three-dimensional time-domain scattering of waves in the marginal ice zone
publisher Royal Society Publishing
publishDate 2018
url http://hdl.handle.net/1959.13/1393615
genre Sea ice
genre_facet Sea ice
op_relation Royal Society of London. Philosophical Transactions A. Mathematical, Physical, and Engineering Sciences Vol. 376, Issue 2129, p. 1-19
10.1098/rsta.2017.0334
op_rights ­© 2018 The Authors. Published by the Royal Society under the terms of the Creative Commons Attribution License http://creativecommons.org/licenses/ by/4.0/, which permits unrestricted use, provided the original author and source are credited.
op_rightsnorm CC-BY
_version_ 1766193189925945344