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Includes abstract.
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| Other Authors: | |
| Format: | Thesis |
| Language: | English |
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Department of Oceanography
2014
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| _version_ | 1867613338799702017 |
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| access_status_str | Open Access |
| author | Halo, Issufo Ferrão Mário |
| author2 | Ansorge, Isabelle Jane |
| author_browse | Ansorge, Isabelle Jane Halo, Issufo Ferrão Mário |
| author_facet | Ansorge, Isabelle Jane Halo, Issufo Ferrão Mário |
| author_sort | Halo, Issufo Ferrão Mário |
| collection | Thesis |
| description | Includes abstract. |
| format | Thesis |
| id | oai:open.uct.ac.za:11427/6478 |
| institution | University of Cape Town (South Africa) |
| language | eng |
| last_indexed | 2026-06-10T12:34:33.896Z |
| license_str | Not specified — see source repository |
| provenance_str_mv | Harvested via OAI-PMH from UCTD — University of Cape Town Open Access Repository |
| publishDate | 2014 |
| publishDateRange | 2014 |
| publishDateSort | 2014 |
| 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:11427/6478 The influence of ocean ridges on the circulation to the south of the Mozambique channel and Madagascar Halo, Issufo Ferrão Mário Ansorge, Isabelle Jane Penven, Pierrick Lutjeharms, Johann R E Oceanography Includes abstract. Includes bibliographical references (leaves 85-92). The Mozambique Channel and the region south of Madagascar are dominated by high variability of the oceanic flow due to the ubiquitous presence of mesoscale eddies. The bottom topography of this region has several shallow ridges. The water flowing through the Mozambique Channel propagates southwards predominantly as a train of anti-cyclonic eddies, moving towards the Agulhas Current. South of Madagascar, dipolar vortices regularly propagate in a south-westward direction. Their deep extent favours interaction with the shallow bathymetry of the Davie, Mozambique and Madagascar Ridges. The role of the Madagascar Ridge on the mesoscale circulation is investigated using altimetric observations and model simulations. 2014-08-13T19:49:03Z 2014-08-13T19:49:03Z 2008 Master Thesis Masters MSc http://hdl.handle.net/11427/6478 eng application/pdf Department of Oceanography Faculty of Science University of Cape Town |
| spellingShingle | Oceanography Halo, Issufo Ferrão Mário The influence of ocean ridges on the circulation to the south of the Mozambique channel and Madagascar |
| thesis_degree_str | Master's |
| title | The influence of ocean ridges on the circulation to the south of the Mozambique channel and Madagascar |
| title_full | The influence of ocean ridges on the circulation to the south of the Mozambique channel and Madagascar |
| title_fullStr | The influence of ocean ridges on the circulation to the south of the Mozambique channel and Madagascar |
| title_full_unstemmed | The influence of ocean ridges on the circulation to the south of the Mozambique channel and Madagascar |
| title_short | The influence of ocean ridges on the circulation to the south of the Mozambique channel and Madagascar |
| title_sort | influence of ocean ridges on the circulation to the south of the mozambique channel and madagascar |
| topic | Oceanography |
| url | http://hdl.handle.net/11427/6478 |
| work_keys_str_mv | AT haloissufoferraomario theinfluenceofoceanridgesonthecirculationtothesouthofthemozambiquechannelandmadagascar AT haloissufoferraomario influenceofoceanridgesonthecirculationtothesouthofthemozambiquechannelandmadagascar |