Linear wave forcing of an array of axisymmetric ice floes

Under linear and time-harmonic conditions, a set of periodic Green's functions is derived to combine the interactions of an infinite number of identical equispaced floating bodies. The bodies themselves are compliant thin elastic plates that can represent ice floes, and unlike previous studies,...

Full description

Bibliographic Details
Published in:IMA Journal of Applied Mathematics
Main Authors: Bennetts, L., Squire, V.
Format: Article in Journal/Newspaper
Language:English
Published: Oxford Univ Press 2010
Subjects:
Online Access:http://hdl.handle.net/2440/75458
https://doi.org/10.1093/imamat/hxp038
id ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/75458
record_format openpolar
spelling ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/75458 2023-12-24T10:24:46+01:00 Linear wave forcing of an array of axisymmetric ice floes Bennetts, L. Squire, V. 2010 http://hdl.handle.net/2440/75458 https://doi.org/10.1093/imamat/hxp038 en eng Oxford Univ Press IMA Journal of Applied Mathematics, 2010; 75(1):108-138 0272-4960 1464-3634 http://hdl.handle.net/2440/75458 doi:10.1093/imamat/hxp038 Bennetts, L. [0000-0001-9386-7882] © The Author 2009. Published by Oxford University Press on behalf of the Institute of Mathematics and its Applications. All rights reserved. http://dx.doi.org/10.1093/imamat/hxp038 Green's function periodic array sea ice flexural-gravity waves scattering Journal article 2010 ftunivadelaidedl https://doi.org/10.1093/imamat/hxp038 2023-11-27T23:19:13Z Under linear and time-harmonic conditions, a set of periodic Green's functions is derived to combine the interactions of an infinite number of identical equispaced floating bodies. The bodies themselves are compliant thin elastic plates that can represent ice floes, and unlike previous studies, they are permitted to vary axisymmetrically in thickness through both their upper and their lower surfaces, with a realistic draught also admitted. Initially, the governing equations are simplified by means of an expansion of the vertical dependence of the unknown velocity potential combined with a variational principle, which reduces calculations to the horizontal plane alone. The unknowns of the resulting equations are written as an integral representation in the free-surface domain and as a Fourier expansion in the domain of the ice-covered fluid, and these are matched at their common boundary to complete the solution process. Our method is validated using numerical results for example problems. The effects of varying the distance between the floes, as well as the introduction of thickness variations and submergence, are also demonstrated. Luke G. Bennetts and Vernon A. Squire Article in Journal/Newspaper Sea ice The University of Adelaide: Digital Library Luke ENVELOPE(-94.855,-94.855,56.296,56.296) IMA Journal of Applied Mathematics 75 1 108 138
institution Open Polar
collection The University of Adelaide: Digital Library
op_collection_id ftunivadelaidedl
language English
topic Green's function
periodic array
sea ice
flexural-gravity waves
scattering
spellingShingle Green's function
periodic array
sea ice
flexural-gravity waves
scattering
Bennetts, L.
Squire, V.
Linear wave forcing of an array of axisymmetric ice floes
topic_facet Green's function
periodic array
sea ice
flexural-gravity waves
scattering
description Under linear and time-harmonic conditions, a set of periodic Green's functions is derived to combine the interactions of an infinite number of identical equispaced floating bodies. The bodies themselves are compliant thin elastic plates that can represent ice floes, and unlike previous studies, they are permitted to vary axisymmetrically in thickness through both their upper and their lower surfaces, with a realistic draught also admitted. Initially, the governing equations are simplified by means of an expansion of the vertical dependence of the unknown velocity potential combined with a variational principle, which reduces calculations to the horizontal plane alone. The unknowns of the resulting equations are written as an integral representation in the free-surface domain and as a Fourier expansion in the domain of the ice-covered fluid, and these are matched at their common boundary to complete the solution process. Our method is validated using numerical results for example problems. The effects of varying the distance between the floes, as well as the introduction of thickness variations and submergence, are also demonstrated. Luke G. Bennetts and Vernon A. Squire
format Article in Journal/Newspaper
author Bennetts, L.
Squire, V.
author_facet Bennetts, L.
Squire, V.
author_sort Bennetts, L.
title Linear wave forcing of an array of axisymmetric ice floes
title_short Linear wave forcing of an array of axisymmetric ice floes
title_full Linear wave forcing of an array of axisymmetric ice floes
title_fullStr Linear wave forcing of an array of axisymmetric ice floes
title_full_unstemmed Linear wave forcing of an array of axisymmetric ice floes
title_sort linear wave forcing of an array of axisymmetric ice floes
publisher Oxford Univ Press
publishDate 2010
url http://hdl.handle.net/2440/75458
https://doi.org/10.1093/imamat/hxp038
long_lat ENVELOPE(-94.855,-94.855,56.296,56.296)
geographic Luke
geographic_facet Luke
genre Sea ice
genre_facet Sea ice
op_source http://dx.doi.org/10.1093/imamat/hxp038
op_relation IMA Journal of Applied Mathematics, 2010; 75(1):108-138
0272-4960
1464-3634
http://hdl.handle.net/2440/75458
doi:10.1093/imamat/hxp038
Bennetts, L. [0000-0001-9386-7882]
op_rights © The Author 2009. Published by Oxford University Press on behalf of the Institute of Mathematics and its Applications. All rights reserved.
op_doi https://doi.org/10.1093/imamat/hxp038
container_title IMA Journal of Applied Mathematics
container_volume 75
container_issue 1
container_start_page 108
op_container_end_page 138
_version_ 1786199888171630592