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Forced synoptic coastal-trapped waves along the southern African coastline

Bibliography: pages 209-221.

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Bibliographic Details
Main Author: Van Ballegooyen, Roy C
Other Authors: Brundrit, Geoff B
Format: Thesis
Language:English
Published: Department of Oceanography 2016
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access_status_str Open Access
author Van Ballegooyen, Roy C
author2 Brundrit, Geoff B
author_browse Brundrit, Geoff B
Van Ballegooyen, Roy C
author_facet Brundrit, Geoff B
Van Ballegooyen, Roy C
author_sort Van Ballegooyen, Roy C
collection Thesis
description Bibliography: pages 209-221.
format Thesis
id oai:open.uct.ac.za:11427/21348
institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:33:31.121Z
license_str Not specified — see source repository
provenance_str_mv Harvested via OAI-PMH from UCTD — University of Cape Town Open Access Repository
publishDate 2016
publishDateRange 2016
publishDateSort 2016
publisher Department of Oceanography
publisherStr Department of Oceanography
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source_str UCTD — University of Cape Town Open Access Repository
spelling oai:open.uct.ac.za:11427/21348 Forced synoptic coastal-trapped waves along the southern African coastline Van Ballegooyen, Roy C Brundrit, Geoff B Oceanography Bibliography: pages 209-221. The presence of subinertial (2 to 20 day) oscillations in sea levels and currents over the continental shelf surrounding southern Africa is well-documented, however presently available observational data alone are largely ~nsuitable or insufficient to adequately characterise the shelf circulation in terms of coastal-trapped wave (CTW) theory. In this dissertation, an analysis of atmospheric pressure and sea level data from 1980 to 1990, a scale analysis of the equations of motion and numerical modelling are used to characterise the subinertial coastal-trapped wave motions off the west coast and south coasts of southern Africa. Appropriate scaling of the equations of motion and numerical analyses of the subinertial CTW response at a number of locations along the west and south coasts of southern Africa indicate that the large scale response of shelf waters to synoptic scale or "weather band" atmospheric forcing is predominantly barotropic. This permits the use of the linear, vertically integrated, shallow water wave equations on a J-plane to model the response of the West Coast shelf waters to "weather band" atmospheric forcing. The CTW dispersion curves have been calculated for a number of shelf profiles along the West and South Coast and are used in the interpretation of the sea level analyses and the numerical modelling results, and further to investigate the effect of increasing water column stratification on the subinertial CTW response 2016-08-18T13:57:47Z 2016-08-18T13:57:47Z 1995 Master Thesis Masters MSc http://hdl.handle.net/11427/21348 eng application/pdf Department of Oceanography Faculty of Science University of Cape Town
spellingShingle Oceanography
Van Ballegooyen, Roy C
Forced synoptic coastal-trapped waves along the southern African coastline
thesis_degree_str Master's
title Forced synoptic coastal-trapped waves along the southern African coastline
title_full Forced synoptic coastal-trapped waves along the southern African coastline
title_fullStr Forced synoptic coastal-trapped waves along the southern African coastline
title_full_unstemmed Forced synoptic coastal-trapped waves along the southern African coastline
title_short Forced synoptic coastal-trapped waves along the southern African coastline
title_sort forced synoptic coastal trapped waves along the southern african coastline
topic Oceanography
url http://hdl.handle.net/11427/21348
work_keys_str_mv AT vanballegooyenroyc forcedsynopticcoastaltrappedwavesalongthesouthernafricancoastline