Modelling the wave-induced collisions of ice floes

The wave-induced collisions and rafting of ice floes are investigated experimentally and theoretically. Results from a series of wave basin experiments are presented. Ice floes are simulated experimentally using thin plastic disks. The first round of experiments focusses on measuring the oscillatory...

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Main Author: Yiew, Lucas Jinliang
Other Authors: Bennetts, Luke, Meylan, Mike, School of Mathematical Sciences
Format: Thesis
Language:unknown
Published: 2017
Subjects:
Online Access:http://hdl.handle.net/2440/105360
https://doi.org/10.4225/55/59261a1950cd6
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spelling ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/105360 2023-05-15T18:18:36+02:00 Modelling the wave-induced collisions of ice floes Yiew, Lucas Jinliang Bennetts, Luke Meylan, Mike School of Mathematical Sciences 2017 application/pdf http://hdl.handle.net/2440/105360 https://doi.org/10.4225/55/59261a1950cd6 unknown http://hdl.handle.net/2440/105360 doi:10.4225/55/59261a1950cd6 sea ice ocean waves hydrodynamics Theses 2017 ftunivadelaidedl https://doi.org/10.4225/55/59261a1950cd6 2023-02-06T07:03:41Z The wave-induced collisions and rafting of ice floes are investigated experimentally and theoretically. Results from a series of wave basin experiments are presented. Ice floes are simulated experimentally using thin plastic disks. The first round of experiments focusses on measuring the oscillatory surge, heave, pitch and drift motions of solitary floes. The second and third rounds of experiments record the motions of two adjacent floes. Rafting is suppressed in the second round, and allowed in the third round. Collision and rafting regimes are identified, and collision behaviours are quantified over a range of incident wavelengths and wave amplitudes. Two mathematical models are proposed to model the wave-induced motions of solitary floes. The first is based on slope-sliding theory, and the second is based on linear potential-ow theory. Both models are validated using results from the single-floe experiments. Model-data comparisons show that the slope-sliding model is valid in the long-wavelength regime, and potential-ow model is more accurate in shorter wavelengths. A two-floe collision model is then developed to replicate the conditions of the two-floe experiments. Slope-sliding theory is used to model floe motions. A time-stepping algorithm is implemented to determine the occurrence of collision and rafting events. Predicted collision behaviours are compared with results from the two-floe experiments. Good agreement is attained in incident waves of intermediate to long wavelengths. Thesis (Ph.D.) -- University of Adelaide, School of Mathematical Sciences, 2017. Thesis Sea ice The University of Adelaide: Digital Library
institution Open Polar
collection The University of Adelaide: Digital Library
op_collection_id ftunivadelaidedl
language unknown
topic sea ice
ocean waves
hydrodynamics
spellingShingle sea ice
ocean waves
hydrodynamics
Yiew, Lucas Jinliang
Modelling the wave-induced collisions of ice floes
topic_facet sea ice
ocean waves
hydrodynamics
description The wave-induced collisions and rafting of ice floes are investigated experimentally and theoretically. Results from a series of wave basin experiments are presented. Ice floes are simulated experimentally using thin plastic disks. The first round of experiments focusses on measuring the oscillatory surge, heave, pitch and drift motions of solitary floes. The second and third rounds of experiments record the motions of two adjacent floes. Rafting is suppressed in the second round, and allowed in the third round. Collision and rafting regimes are identified, and collision behaviours are quantified over a range of incident wavelengths and wave amplitudes. Two mathematical models are proposed to model the wave-induced motions of solitary floes. The first is based on slope-sliding theory, and the second is based on linear potential-ow theory. Both models are validated using results from the single-floe experiments. Model-data comparisons show that the slope-sliding model is valid in the long-wavelength regime, and potential-ow model is more accurate in shorter wavelengths. A two-floe collision model is then developed to replicate the conditions of the two-floe experiments. Slope-sliding theory is used to model floe motions. A time-stepping algorithm is implemented to determine the occurrence of collision and rafting events. Predicted collision behaviours are compared with results from the two-floe experiments. Good agreement is attained in incident waves of intermediate to long wavelengths. Thesis (Ph.D.) -- University of Adelaide, School of Mathematical Sciences, 2017.
author2 Bennetts, Luke
Meylan, Mike
School of Mathematical Sciences
format Thesis
author Yiew, Lucas Jinliang
author_facet Yiew, Lucas Jinliang
author_sort Yiew, Lucas Jinliang
title Modelling the wave-induced collisions of ice floes
title_short Modelling the wave-induced collisions of ice floes
title_full Modelling the wave-induced collisions of ice floes
title_fullStr Modelling the wave-induced collisions of ice floes
title_full_unstemmed Modelling the wave-induced collisions of ice floes
title_sort modelling the wave-induced collisions of ice floes
publishDate 2017
url http://hdl.handle.net/2440/105360
https://doi.org/10.4225/55/59261a1950cd6
genre Sea ice
genre_facet Sea ice
op_relation http://hdl.handle.net/2440/105360
doi:10.4225/55/59261a1950cd6
op_doi https://doi.org/10.4225/55/59261a1950cd6
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