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The influence of ocean ridges on the circulation to the south of the Mozambique channel and Madagascar

Includes abstract.

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Bibliographic Details
Main Author: Halo, Issufo Ferrão Mário
Other Authors: Ansorge, Isabelle Jane
Format: Thesis
Language:English
Published: Department of Oceanography 2014
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_version_ 1867613338799702017
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
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AT haloissufoferraomario influenceofoceanridgesonthecirculationtothesouthofthemozambiquechannelandmadagascar