Interaction of ocean wave with a harbor covered by an ice sheet

A domain decomposition method is developed to solve the problem of wave motion inside a harbor with its surface covered by an ice sheet. The shape of the horizontal plane of the harbor can be arbitrary while the sidewall is vertical. The entrance of the harbor is open to the sea with a free surface....

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Published in:Physics of Fluids
Main Authors: Li, Z. F., Shi, Y. Y., Wu, G. X.
Other Authors: Lloyd's Register Foundation, National Natural Science Foundation of China
Format: Article in Journal/Newspaper
Language:English
Published: AIP Publishing 2021
Subjects:
Online Access:http://dx.doi.org/10.1063/5.0051376
https://pubs.aip.org/aip/pof/article-pdf/doi/10.1063/5.0051376/19763235/057109_1_online.pdf
id craippubl:10.1063/5.0051376
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spelling craippubl:10.1063/5.0051376 2024-06-23T07:53:45+00:00 Interaction of ocean wave with a harbor covered by an ice sheet Li, Z. F. Shi, Y. Y. Wu, G. X. Lloyd's Register Foundation National Natural Science Foundation of China National Natural Science Foundation of China National Natural Science Foundation of China National Natural Science Foundation of China 2021 http://dx.doi.org/10.1063/5.0051376 https://pubs.aip.org/aip/pof/article-pdf/doi/10.1063/5.0051376/19763235/057109_1_online.pdf en eng AIP Publishing Physics of Fluids volume 33, issue 5 ISSN 1070-6631 1089-7666 journal-article 2021 craippubl https://doi.org/10.1063/5.0051376 2024-06-13T04:04:31Z A domain decomposition method is developed to solve the problem of wave motion inside a harbor with its surface covered by an ice sheet. The shape of the horizontal plane of the harbor can be arbitrary while the sidewall is vertical. The entrance of the harbor is open to the sea with a free surface. The linearized velocity potential theory is adopted for fluid flow, and the thin elastic plate model is applied for the ice sheet. The domain is divided into two subdomains. Inside the harbor, the velocity potential is expanded into a series of eigenfunctions in the vertical direction. The orthogonal inner product is adopted to impose the impermeable condition on the harbor wall, together with the edge conditions on the intersection of the harbor wall and the ice sheet. In the open sea outside of the harbor, through the modified Green function, the velocity potential is written in terms of an integral equation over the surface of the harbor entrance, or the interface between the two subdomains. On the interface, the orthogonal inner product is also applied to impose the continuity conditions of velocity and pressure as well as the free ice edge conditions. Computations are first carried out for a rectangular harbor without the ice sheet to verify the methodology, and then extensive results and discussions are provided for a harbor of a more general shape covered by an ice sheet with different thicknesses and under different incident wave angles. Article in Journal/Newspaper Ice Sheet AIP Publishing Physics of Fluids 33 5 057109
institution Open Polar
collection AIP Publishing
op_collection_id craippubl
language English
description A domain decomposition method is developed to solve the problem of wave motion inside a harbor with its surface covered by an ice sheet. The shape of the horizontal plane of the harbor can be arbitrary while the sidewall is vertical. The entrance of the harbor is open to the sea with a free surface. The linearized velocity potential theory is adopted for fluid flow, and the thin elastic plate model is applied for the ice sheet. The domain is divided into two subdomains. Inside the harbor, the velocity potential is expanded into a series of eigenfunctions in the vertical direction. The orthogonal inner product is adopted to impose the impermeable condition on the harbor wall, together with the edge conditions on the intersection of the harbor wall and the ice sheet. In the open sea outside of the harbor, through the modified Green function, the velocity potential is written in terms of an integral equation over the surface of the harbor entrance, or the interface between the two subdomains. On the interface, the orthogonal inner product is also applied to impose the continuity conditions of velocity and pressure as well as the free ice edge conditions. Computations are first carried out for a rectangular harbor without the ice sheet to verify the methodology, and then extensive results and discussions are provided for a harbor of a more general shape covered by an ice sheet with different thicknesses and under different incident wave angles.
author2 Lloyd's Register Foundation
National Natural Science Foundation of China
National Natural Science Foundation of China
National Natural Science Foundation of China
National Natural Science Foundation of China
format Article in Journal/Newspaper
author Li, Z. F.
Shi, Y. Y.
Wu, G. X.
spellingShingle Li, Z. F.
Shi, Y. Y.
Wu, G. X.
Interaction of ocean wave with a harbor covered by an ice sheet
author_facet Li, Z. F.
Shi, Y. Y.
Wu, G. X.
author_sort Li, Z. F.
title Interaction of ocean wave with a harbor covered by an ice sheet
title_short Interaction of ocean wave with a harbor covered by an ice sheet
title_full Interaction of ocean wave with a harbor covered by an ice sheet
title_fullStr Interaction of ocean wave with a harbor covered by an ice sheet
title_full_unstemmed Interaction of ocean wave with a harbor covered by an ice sheet
title_sort interaction of ocean wave with a harbor covered by an ice sheet
publisher AIP Publishing
publishDate 2021
url http://dx.doi.org/10.1063/5.0051376
https://pubs.aip.org/aip/pof/article-pdf/doi/10.1063/5.0051376/19763235/057109_1_online.pdf
genre Ice Sheet
genre_facet Ice Sheet
op_source Physics of Fluids
volume 33, issue 5
ISSN 1070-6631 1089-7666
op_doi https://doi.org/10.1063/5.0051376
container_title Physics of Fluids
container_volume 33
container_issue 5
container_start_page 057109
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