A study of wind stress and boundary effects on sea level and coastal currents

This thesis includes both a discussion of free and forced topographic trapped edge waves over various continental shelf profiles, and an examination of the boundary effects on sea level coastal current movement through a strait or channel. Using the linearized long wave theory and the methods of com...

Full description

Bibliographic Details
Main Author: Worthy, A. L.
Format: Thesis
Language:unknown
Published: Department of Mathematics 1989
Subjects:
Online Access:https://ro.uow.edu.au/theses/1541
https://ro.uow.edu.au/cgi/viewcontent.cgi?article=2541&context=theses
id ftunivwollongong:oai:ro.uow.edu.au:theses-2541
record_format openpolar
spelling ftunivwollongong:oai:ro.uow.edu.au:theses-2541 2023-05-15T18:27:31+02:00 A study of wind stress and boundary effects on sea level and coastal currents Worthy, A. L. 1989-01-01T08:00:00Z application/pdf https://ro.uow.edu.au/theses/1541 https://ro.uow.edu.au/cgi/viewcontent.cgi?article=2541&context=theses unknown Department of Mathematics https://ro.uow.edu.au/theses/1541 https://ro.uow.edu.au/cgi/viewcontent.cgi?article=2541&context=theses University of Wollongong Thesis Collection 1954-2016 thesis 1989 ftunivwollongong 2021-11-08T23:30:55Z This thesis includes both a discussion of free and forced topographic trapped edge waves over various continental shelf profiles, and an examination of the boundary effects on sea level coastal current movement through a strait or channel. Using the linearized long wave theory and the methods of complex analysis, edge wave solutions are analytically determined over a linear and exponential, finite and semi-infinite, continental shelf profile. The effects of both pressure and wind stress forcing of edge waves also discussed. An analysis of wind generated Class I and Class II edge waves is included, along with a comparison of the analytical results with the physical data obtained from current meter recordings taken along the south eastern coast of Australia. It is shown that the analytical compare favourably with the physical results. A discussion of the applications of various open boundary methods, including the relatively new Characteristic method, to current flow through a strait or channel is included so that the methods can be compared when applied to the Strait of Belle Isle, Canada. A numerical model the Strait of Belle Isle is used to examine the effect various boundary conditions have on current flow through a strait or channel. The results obtained by using the Characteristic method, the gradient method, and specifying sea level values along the open boundary are compared and it shown that the Characteristic method gives what could be considered very 'realistic' results. Thesis Strait of Belle Isle University of Wollongong, Australia: Research Online Belle Isle ENVELOPE(-55.357,-55.357,51.942,51.942) Canada Strait of Belle Isle ENVELOPE(-57.115,-57.115,51.400,51.400)
institution Open Polar
collection University of Wollongong, Australia: Research Online
op_collection_id ftunivwollongong
language unknown
description This thesis includes both a discussion of free and forced topographic trapped edge waves over various continental shelf profiles, and an examination of the boundary effects on sea level coastal current movement through a strait or channel. Using the linearized long wave theory and the methods of complex analysis, edge wave solutions are analytically determined over a linear and exponential, finite and semi-infinite, continental shelf profile. The effects of both pressure and wind stress forcing of edge waves also discussed. An analysis of wind generated Class I and Class II edge waves is included, along with a comparison of the analytical results with the physical data obtained from current meter recordings taken along the south eastern coast of Australia. It is shown that the analytical compare favourably with the physical results. A discussion of the applications of various open boundary methods, including the relatively new Characteristic method, to current flow through a strait or channel is included so that the methods can be compared when applied to the Strait of Belle Isle, Canada. A numerical model the Strait of Belle Isle is used to examine the effect various boundary conditions have on current flow through a strait or channel. The results obtained by using the Characteristic method, the gradient method, and specifying sea level values along the open boundary are compared and it shown that the Characteristic method gives what could be considered very 'realistic' results.
format Thesis
author Worthy, A. L.
spellingShingle Worthy, A. L.
A study of wind stress and boundary effects on sea level and coastal currents
author_facet Worthy, A. L.
author_sort Worthy, A. L.
title A study of wind stress and boundary effects on sea level and coastal currents
title_short A study of wind stress and boundary effects on sea level and coastal currents
title_full A study of wind stress and boundary effects on sea level and coastal currents
title_fullStr A study of wind stress and boundary effects on sea level and coastal currents
title_full_unstemmed A study of wind stress and boundary effects on sea level and coastal currents
title_sort study of wind stress and boundary effects on sea level and coastal currents
publisher Department of Mathematics
publishDate 1989
url https://ro.uow.edu.au/theses/1541
https://ro.uow.edu.au/cgi/viewcontent.cgi?article=2541&context=theses
long_lat ENVELOPE(-55.357,-55.357,51.942,51.942)
ENVELOPE(-57.115,-57.115,51.400,51.400)
geographic Belle Isle
Canada
Strait of Belle Isle
geographic_facet Belle Isle
Canada
Strait of Belle Isle
genre Strait of Belle Isle
genre_facet Strait of Belle Isle
op_source University of Wollongong Thesis Collection 1954-2016
op_relation https://ro.uow.edu.au/theses/1541
https://ro.uow.edu.au/cgi/viewcontent.cgi?article=2541&context=theses
_version_ 1766209627155857408