Drift of elastic floating ice sheets by waves and current, part I: single sheet

The drift motion of a freely floating deformable ice sheet in shallow water subjected to incident nonlinear waves and uniform current is studied by use of the Green–Naghdi theory for the fluid motion and the thin plate theory for an elastic sheet. The nonlinear wave- and current-induced forces are o...

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Published in:Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences
Main Authors: Kostikov, Vasily K., Hayatdavoodi, Masoud, Ertekin, R. C.
Format: Article in Journal/Newspaper
Language:English
Published: The Royal Society 2021
Subjects:
Online Access:http://dx.doi.org/10.1098/rspa.2021.0449
https://royalsocietypublishing.org/doi/pdf/10.1098/rspa.2021.0449
https://royalsocietypublishing.org/doi/full-xml/10.1098/rspa.2021.0449
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spelling crroyalsociety:10.1098/rspa.2021.0449 2024-06-02T08:08:17+00:00 Drift of elastic floating ice sheets by waves and current, part I: single sheet Kostikov, Vasily K. Hayatdavoodi, Masoud Ertekin, R. C. 2021 http://dx.doi.org/10.1098/rspa.2021.0449 https://royalsocietypublishing.org/doi/pdf/10.1098/rspa.2021.0449 https://royalsocietypublishing.org/doi/full-xml/10.1098/rspa.2021.0449 en eng The Royal Society https://royalsociety.org/journals/ethics-policies/data-sharing-mining/ Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences volume 477, issue 2254 ISSN 1364-5021 1471-2946 journal-article 2021 crroyalsociety https://doi.org/10.1098/rspa.2021.0449 2024-05-07T14:16:47Z The drift motion of a freely floating deformable ice sheet in shallow water subjected to incident nonlinear waves and uniform current is studied by use of the Green–Naghdi theory for the fluid motion and the thin plate theory for an elastic sheet. The nonlinear wave- and current-induced forces are obtained by integrating the hydrodynamic pressure around the body. The oscillations and translational motion of the sheet are then determined by substituting the flow-induced forces into the equation of motion of the body. The resulting governing equations, boundary and matching conditions are solved in two dimensions with a finite difference technique. The surge and drift motions of the sheet are analysed in a broad range of body parameters and various wave-current conditions. It is demonstrated that wavelength to sheet length ratio plays an important role in the drift response of the floating sheet, while the sheet mass and rigidity have comparatively less impact. It is also observed that while the presence of the ambient current changes the drift speed significantly (almost linearly), it has little to no effect on its oscillations. However, under the same ambient current, the drift speed changes remarkably by the wave period (or wavelength). Article in Journal/Newspaper Ice Sheet The Royal Society Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences 477 2254
institution Open Polar
collection The Royal Society
op_collection_id crroyalsociety
language English
description The drift motion of a freely floating deformable ice sheet in shallow water subjected to incident nonlinear waves and uniform current is studied by use of the Green–Naghdi theory for the fluid motion and the thin plate theory for an elastic sheet. The nonlinear wave- and current-induced forces are obtained by integrating the hydrodynamic pressure around the body. The oscillations and translational motion of the sheet are then determined by substituting the flow-induced forces into the equation of motion of the body. The resulting governing equations, boundary and matching conditions are solved in two dimensions with a finite difference technique. The surge and drift motions of the sheet are analysed in a broad range of body parameters and various wave-current conditions. It is demonstrated that wavelength to sheet length ratio plays an important role in the drift response of the floating sheet, while the sheet mass and rigidity have comparatively less impact. It is also observed that while the presence of the ambient current changes the drift speed significantly (almost linearly), it has little to no effect on its oscillations. However, under the same ambient current, the drift speed changes remarkably by the wave period (or wavelength).
format Article in Journal/Newspaper
author Kostikov, Vasily K.
Hayatdavoodi, Masoud
Ertekin, R. C.
spellingShingle Kostikov, Vasily K.
Hayatdavoodi, Masoud
Ertekin, R. C.
Drift of elastic floating ice sheets by waves and current, part I: single sheet
author_facet Kostikov, Vasily K.
Hayatdavoodi, Masoud
Ertekin, R. C.
author_sort Kostikov, Vasily K.
title Drift of elastic floating ice sheets by waves and current, part I: single sheet
title_short Drift of elastic floating ice sheets by waves and current, part I: single sheet
title_full Drift of elastic floating ice sheets by waves and current, part I: single sheet
title_fullStr Drift of elastic floating ice sheets by waves and current, part I: single sheet
title_full_unstemmed Drift of elastic floating ice sheets by waves and current, part I: single sheet
title_sort drift of elastic floating ice sheets by waves and current, part i: single sheet
publisher The Royal Society
publishDate 2021
url http://dx.doi.org/10.1098/rspa.2021.0449
https://royalsocietypublishing.org/doi/pdf/10.1098/rspa.2021.0449
https://royalsocietypublishing.org/doi/full-xml/10.1098/rspa.2021.0449
genre Ice Sheet
genre_facet Ice Sheet
op_source Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences
volume 477, issue 2254
ISSN 1364-5021 1471-2946
op_rights https://royalsociety.org/journals/ethics-policies/data-sharing-mining/
op_doi https://doi.org/10.1098/rspa.2021.0449
container_title Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences
container_volume 477
container_issue 2254
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