Wave diffraction by multiple arbitrary shaped cracks in an infinitely extended ice sheet of finite water depth

lexural-gravity wave interactions with multiple cracks in an ice sheet of infinite extent are considered, based on the linearized velocity potential theory for fluid flow and thin elastic plate model for an ice sheet. Both the shape and location of the cracks can be arbitrary, while an individual cr...

Full description

Bibliographic Details
Main Authors: Li, ZF, Wu, GX, Ren, K
Format: Article in Journal/Newspaper
Language:unknown
Published: CAMBRIDGE UNIV PRESS 2020
Subjects:
Online Access:https://discovery.ucl.ac.uk/id/eprint/10097413/1/MainDocument%20%28003%29.pdf
https://discovery.ucl.ac.uk/id/eprint/10097413/
id ftucl:oai:eprints.ucl.ac.uk.OAI2:10097413
record_format openpolar
spelling ftucl:oai:eprints.ucl.ac.uk.OAI2:10097413 2023-12-24T10:17:35+01:00 Wave diffraction by multiple arbitrary shaped cracks in an infinitely extended ice sheet of finite water depth Li, ZF Wu, GX Ren, K 2020-06-25 text https://discovery.ucl.ac.uk/id/eprint/10097413/1/MainDocument%20%28003%29.pdf https://discovery.ucl.ac.uk/id/eprint/10097413/ unknown CAMBRIDGE UNIV PRESS https://discovery.ucl.ac.uk/id/eprint/10097413/1/MainDocument%20%28003%29.pdf https://discovery.ucl.ac.uk/id/eprint/10097413/ open Journal of Fluid Mechanics , 893 , Article A14. (2020) ice sheets surface gravity waves wave scattering Article 2020 ftucl 2023-11-27T13:07:35Z lexural-gravity wave interactions with multiple cracks in an ice sheet of infinite extent are considered, based on the linearized velocity potential theory for fluid flow and thin elastic plate model for an ice sheet. Both the shape and location of the cracks can be arbitrary, while an individual crack can be either open or closed. Free edge conditions are imposed at the crack. For open cracks, zero corner force conditions are further applied at the crack tips. The solution procedure starts from series expansion in the vertical direction based on separation of variables, which decomposes the three-dimensional problem into an infinite number of coupled two-dimensional problems in the horizontal plane. For each two-dimensional problem, an integral equation is derived along the cracks, with the jumps of displacement and slope of the ice sheet as unknowns in the integrand. By extending the crack in the vertical direction into the fluid domain, an artificial vertical surface is formed, on which an orthogonal inner product is adopted for the vertical modes. Through this, the edge conditions at the cracks are satisfied, together with continuous conditions of pressure and velocity on the vertical surface. The integral differential equations are solved numerically through the boundary element method together with the finite difference scheme for the derivatives along the crack. Extensive results are provided and analysed for cracks with various shapes and locations, including the jumps of displacement and slope, diffraction wave coefficient, and the scattered cross-section. Article in Journal/Newspaper Ice Sheet University College London: UCL Discovery
institution Open Polar
collection University College London: UCL Discovery
op_collection_id ftucl
language unknown
topic ice sheets
surface gravity waves
wave scattering
spellingShingle ice sheets
surface gravity waves
wave scattering
Li, ZF
Wu, GX
Ren, K
Wave diffraction by multiple arbitrary shaped cracks in an infinitely extended ice sheet of finite water depth
topic_facet ice sheets
surface gravity waves
wave scattering
description lexural-gravity wave interactions with multiple cracks in an ice sheet of infinite extent are considered, based on the linearized velocity potential theory for fluid flow and thin elastic plate model for an ice sheet. Both the shape and location of the cracks can be arbitrary, while an individual crack can be either open or closed. Free edge conditions are imposed at the crack. For open cracks, zero corner force conditions are further applied at the crack tips. The solution procedure starts from series expansion in the vertical direction based on separation of variables, which decomposes the three-dimensional problem into an infinite number of coupled two-dimensional problems in the horizontal plane. For each two-dimensional problem, an integral equation is derived along the cracks, with the jumps of displacement and slope of the ice sheet as unknowns in the integrand. By extending the crack in the vertical direction into the fluid domain, an artificial vertical surface is formed, on which an orthogonal inner product is adopted for the vertical modes. Through this, the edge conditions at the cracks are satisfied, together with continuous conditions of pressure and velocity on the vertical surface. The integral differential equations are solved numerically through the boundary element method together with the finite difference scheme for the derivatives along the crack. Extensive results are provided and analysed for cracks with various shapes and locations, including the jumps of displacement and slope, diffraction wave coefficient, and the scattered cross-section.
format Article in Journal/Newspaper
author Li, ZF
Wu, GX
Ren, K
author_facet Li, ZF
Wu, GX
Ren, K
author_sort Li, ZF
title Wave diffraction by multiple arbitrary shaped cracks in an infinitely extended ice sheet of finite water depth
title_short Wave diffraction by multiple arbitrary shaped cracks in an infinitely extended ice sheet of finite water depth
title_full Wave diffraction by multiple arbitrary shaped cracks in an infinitely extended ice sheet of finite water depth
title_fullStr Wave diffraction by multiple arbitrary shaped cracks in an infinitely extended ice sheet of finite water depth
title_full_unstemmed Wave diffraction by multiple arbitrary shaped cracks in an infinitely extended ice sheet of finite water depth
title_sort wave diffraction by multiple arbitrary shaped cracks in an infinitely extended ice sheet of finite water depth
publisher CAMBRIDGE UNIV PRESS
publishDate 2020
url https://discovery.ucl.ac.uk/id/eprint/10097413/1/MainDocument%20%28003%29.pdf
https://discovery.ucl.ac.uk/id/eprint/10097413/
genre Ice Sheet
genre_facet Ice Sheet
op_source Journal of Fluid Mechanics , 893 , Article A14. (2020)
op_relation https://discovery.ucl.ac.uk/id/eprint/10097413/1/MainDocument%20%28003%29.pdf
https://discovery.ucl.ac.uk/id/eprint/10097413/
op_rights open
_version_ 1786205829879300096