Wave induced motion of small ice masses

Thesis (M.Eng.)--Memorial University of Newfoundland, 1987. Engineering and Applied Science Bibliography: leaves 126-128. Experiments have been performed to assess the ability of linear diffraction theory to predict the motion of ice masses under wave excitation. Variables in the regular wave portio...

Full description

Bibliographic Details
Main Author: Attwood, Daryl
Other Authors: Memorial University of Newfoundland. Faculty of Engineering and Applied Science
Format: Thesis
Language:English
Published: 1986
Subjects:
Online Access:http://collections.mun.ca/cdm/ref/collection/theses2/id/271046
id ftmemorialunivdc:oai:collections.mun.ca:theses2/271046
record_format openpolar
spelling ftmemorialunivdc:oai:collections.mun.ca:theses2/271046 2023-05-15T17:23:31+02:00 Wave induced motion of small ice masses Attwood, Daryl Memorial University of Newfoundland. Faculty of Engineering and Applied Science 1986 viii, 255 leaves : ill. Image/jpeg; Application/pdf http://collections.mun.ca/cdm/ref/collection/theses2/id/271046 Eng eng Electronic Theses and Dissertations (25.59 MB) -- http://collections.mun.ca/PDFs/theses/Attwood_Daryl.pdf 75414564 http://collections.mun.ca/cdm/ref/collection/theses2/id/271046 The author retains copyright ownership and moral rights in this thesis. Neither the thesis nor substantial extracts from it may be printed or otherwise reproduced without the author's permission. Paper copy kept in the Centre for Newfoundland Studies, Memorial University Libraries Ice--Dynamics Sea ice--Dynamics Waves Text Electronic thesis or dissertation 1986 ftmemorialunivdc 2015-08-06T19:17:32Z Thesis (M.Eng.)--Memorial University of Newfoundland, 1987. Engineering and Applied Science Bibliography: leaves 126-128. Experiments have been performed to assess the ability of linear diffraction theory to predict the motion of ice masses under wave excitation. Variables in the regular wave portion of the experiment included iceberg size and shape and wave steepness. Regular wave tests demonstrated accurate motion prediction, with best results achieved for smooth sided bodies undergoing small amplitude motion. Accuracy was lower for low frequency surge and heave resonance results, and generally for bodies with steeply sloping sides. -- Irregular tests were performed to demonstrate the ability to predict motion in an irregular seaway. It was seen that by combining response amplitude operators (RAO's) with wave spectra, response spectra for individual bodies could be predicted. The predicted spectra generated using experimentally determined RAO's very accurately mirrored the ones generated by transforming irregular-wave body response data to the frequency domain. Predicted spectra generated using theoretically determined RAO's were studied as well. It was found that the accuracy of such spectra was directly tied to the accuracy of the associated RAO's. Thesis Newfoundland studies Sea ice University of Newfoundland Memorial University of Newfoundland: Digital Archives Initiative (DAI)
institution Open Polar
collection Memorial University of Newfoundland: Digital Archives Initiative (DAI)
op_collection_id ftmemorialunivdc
language English
topic Ice--Dynamics
Sea ice--Dynamics
Waves
spellingShingle Ice--Dynamics
Sea ice--Dynamics
Waves
Attwood, Daryl
Wave induced motion of small ice masses
topic_facet Ice--Dynamics
Sea ice--Dynamics
Waves
description Thesis (M.Eng.)--Memorial University of Newfoundland, 1987. Engineering and Applied Science Bibliography: leaves 126-128. Experiments have been performed to assess the ability of linear diffraction theory to predict the motion of ice masses under wave excitation. Variables in the regular wave portion of the experiment included iceberg size and shape and wave steepness. Regular wave tests demonstrated accurate motion prediction, with best results achieved for smooth sided bodies undergoing small amplitude motion. Accuracy was lower for low frequency surge and heave resonance results, and generally for bodies with steeply sloping sides. -- Irregular tests were performed to demonstrate the ability to predict motion in an irregular seaway. It was seen that by combining response amplitude operators (RAO's) with wave spectra, response spectra for individual bodies could be predicted. The predicted spectra generated using experimentally determined RAO's very accurately mirrored the ones generated by transforming irregular-wave body response data to the frequency domain. Predicted spectra generated using theoretically determined RAO's were studied as well. It was found that the accuracy of such spectra was directly tied to the accuracy of the associated RAO's.
author2 Memorial University of Newfoundland. Faculty of Engineering and Applied Science
format Thesis
author Attwood, Daryl
author_facet Attwood, Daryl
author_sort Attwood, Daryl
title Wave induced motion of small ice masses
title_short Wave induced motion of small ice masses
title_full Wave induced motion of small ice masses
title_fullStr Wave induced motion of small ice masses
title_full_unstemmed Wave induced motion of small ice masses
title_sort wave induced motion of small ice masses
publishDate 1986
url http://collections.mun.ca/cdm/ref/collection/theses2/id/271046
genre Newfoundland studies
Sea ice
University of Newfoundland
genre_facet Newfoundland studies
Sea ice
University of Newfoundland
op_source Paper copy kept in the Centre for Newfoundland Studies, Memorial University Libraries
op_relation Electronic Theses and Dissertations
(25.59 MB) -- http://collections.mun.ca/PDFs/theses/Attwood_Daryl.pdf
75414564
http://collections.mun.ca/cdm/ref/collection/theses2/id/271046
op_rights The author retains copyright ownership and moral rights in this thesis. Neither the thesis nor substantial extracts from it may be printed or otherwise reproduced without the author's permission.
_version_ 1766113022555717632