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Includes abstract.
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| Format: | Thesis |
| Language: | English |
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Department of Oceanography
2015
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| _version_ | 1867613226413326336 |
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| access_status_str | Open Access |
| author | Veitch, Jennifer Anne |
| author2 | Shillington, Frank |
| author_browse | Shillington, Frank Veitch, Jennifer Anne |
| author_facet | Shillington, Frank Veitch, Jennifer Anne |
| author_sort | Veitch, Jennifer Anne |
| collection | Thesis |
| description | Includes abstract. |
| format | Thesis |
| id | oai:open.uct.ac.za:11427/12153 |
| institution | University of Cape Town (South Africa) |
| language | eng |
| last_indexed | 2026-06-10T12:32:46.693Z |
| license_str | Not specified — see source repository |
| provenance_str_mv | Harvested via OAI-PMH from UCTD — University of Cape Town Open Access Repository |
| publishDate | 2015 |
| publishDateRange | 2015 |
| publishDateSort | 2015 |
| publisher | Department of Oceanography |
| publisherStr | Department of Oceanography |
| record_format | dspace |
| source_str | UCTD — University of Cape Town Open Access Repository |
| spelling | oai:open.uct.ac.za:11427/12153 Equilibrium dynamics of the Benguela system : a numerical modelling approach Veitch, Jennifer Anne Shillington, Frank Penven, Pierrick Oceanography Includes abstract. Includes bibliographical references (p. 237-255). The Regional Ocean Modelling System (ROMS) is used to systematically investigate equilibrium conditions and seasonal variations of the Benguela system, including both the large-scale flow regime as well as the coastal upswelling regime. A shelf-edge poleward flow exists in the northern Benguela region and is driven primarily by the wind-stress curl via the Sverdup relation. As such, it is strongly seasonal and is most intense during spring and summer when the wind-stress curl is most negative. The poleward flow deepens as it moves southward and between 25-27° much of it veers offshore due to the nature of of the wind-stress curl. In the mean state, the Benguela Current is characterized by two streams: the more inshore stream is topographically controlled and follows the run of the shelf-edge. The offshore stream is driven by nonlinear reactions of passing Aghulas rings and eddies and does not have a striking seasonal signal. The model simulates all seven of the major upswelling cells within its domain. 2015-01-13T04:07:59Z 2015-01-13T04:07:59Z 2009 Doctoral Thesis Doctoral PhD http://hdl.handle.net/11427/12153 eng application/pdf Department of Oceanography Faculty of Science University of Cape Town |
| spellingShingle | Oceanography Veitch, Jennifer Anne Equilibrium dynamics of the Benguela system : a numerical modelling approach |
| thesis_degree_str | Doctoral |
| title | Equilibrium dynamics of the Benguela system : a numerical modelling approach |
| title_full | Equilibrium dynamics of the Benguela system : a numerical modelling approach |
| title_fullStr | Equilibrium dynamics of the Benguela system : a numerical modelling approach |
| title_full_unstemmed | Equilibrium dynamics of the Benguela system : a numerical modelling approach |
| title_short | Equilibrium dynamics of the Benguela system : a numerical modelling approach |
| title_sort | equilibrium dynamics of the benguela system a numerical modelling approach |
| topic | Oceanography |
| url | http://hdl.handle.net/11427/12153 |
| work_keys_str_mv | AT veitchjenniferanne equilibriumdynamicsofthebenguelasystemanumericalmodellingapproach |