Matlab code to produce the figures from 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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Bibliographic Details
Main Authors: M. H. Meylan, L. G. Bennetts
Format: Dataset
Language:unknown
Published: The Royal Society 2018
Subjects:
Online Access:https://dx.doi.org/10.6084/m9.figshare.6756635
https://rs.figshare.com/articles/Matlab_code_to_produce_the_figures_from_Three-dimensional_time-domain_scattering_of_waves_in_the_marginal_ice_zone/6756635
id ftdatacite:10.6084/m9.figshare.6756635
record_format openpolar
spelling ftdatacite:10.6084/m9.figshare.6756635 2023-05-15T18:18:31+02:00 Matlab code to produce the figures from Three-dimensional time-domain scattering of waves in the marginal ice zone M. H. Meylan L. G. Bennetts 2018 https://dx.doi.org/10.6084/m9.figshare.6756635 https://rs.figshare.com/articles/Matlab_code_to_produce_the_figures_from_Three-dimensional_time-domain_scattering_of_waves_in_the_marginal_ice_zone/6756635 unknown The Royal Society https://dx.doi.org/10.1098/rsta.2017.0334 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Geophysics FOS Earth and related environmental sciences 10299 Applied Mathematics not elsewhere classified FOS Mathematics dataset Dataset 2018 ftdatacite https://doi.org/10.6084/m9.figshare.6756635 https://doi.org/10.1098/rsta.2017.0334 2021-11-05T12:55:41Z 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’. Dataset Sea ice DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Geophysics
FOS Earth and related environmental sciences
10299 Applied Mathematics not elsewhere classified
FOS Mathematics
spellingShingle Geophysics
FOS Earth and related environmental sciences
10299 Applied Mathematics not elsewhere classified
FOS Mathematics
M. H. Meylan
L. G. Bennetts
Matlab code to produce the figures from Three-dimensional time-domain scattering of waves in the marginal ice zone
topic_facet Geophysics
FOS Earth and related environmental sciences
10299 Applied Mathematics not elsewhere classified
FOS Mathematics
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’.
format Dataset
author M. H. Meylan
L. G. Bennetts
author_facet M. H. Meylan
L. G. Bennetts
author_sort M. H. Meylan
title Matlab code to produce the figures from Three-dimensional time-domain scattering of waves in the marginal ice zone
title_short Matlab code to produce the figures from Three-dimensional time-domain scattering of waves in the marginal ice zone
title_full Matlab code to produce the figures from Three-dimensional time-domain scattering of waves in the marginal ice zone
title_fullStr Matlab code to produce the figures from Three-dimensional time-domain scattering of waves in the marginal ice zone
title_full_unstemmed Matlab code to produce the figures from Three-dimensional time-domain scattering of waves in the marginal ice zone
title_sort matlab code to produce the figures from three-dimensional time-domain scattering of waves in the marginal ice zone
publisher The Royal Society
publishDate 2018
url https://dx.doi.org/10.6084/m9.figshare.6756635
https://rs.figshare.com/articles/Matlab_code_to_produce_the_figures_from_Three-dimensional_time-domain_scattering_of_waves_in_the_marginal_ice_zone/6756635
genre Sea ice
genre_facet Sea ice
op_relation https://dx.doi.org/10.1098/rsta.2017.0334
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.6084/m9.figshare.6756635
https://doi.org/10.1098/rsta.2017.0334
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