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The dynamics and physical processes of the Comoros Basin

Includes abstract.

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Bibliographic Details
Main Author: Collins, Charine
Other Authors: Reason, Chris
Format: Thesis
Language:English
Published: Department of Oceanography 2014
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access_status_str Open Access
author Collins, Charine
author2 Reason, Chris
author_browse Collins, Charine
Reason, Chris
author_facet Reason, Chris
Collins, Charine
author_sort Collins, Charine
collection Thesis
description Includes abstract.
format Thesis
id oai:open.uct.ac.za:11427/6467
institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:53:27.831Z
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:11427/6467 The dynamics and physical processes of the Comoros Basin Collins, Charine Reason, Chris Hermes, Juliet C Oceanography Includes abstract. Includes bibliographical references. The main objective of this thesis was to investigate the circulation in the ComorosBasin using observed and model datasets. These data were used to establish whether or not a Comoros Gyre exists and to investigate the nature of the eddy variability in the basin.The water masses in the Comoros Basin emulate those found further south in the Mozambique Channel. The presence of AAIW north of Madagascar confirmed that this water mass enters the Comoros Basin from the east while the presence of North Atlantic Deep Water showed that this water mass is capable of spreading northward over the Davie Ridge. The main currents in the Comoros Basin, the westward flowing NEMC and a poleward current along the western boundary, are under the influence of the monsoon winds. The NEMC intensifies during the Southwest monsoon in response to a strong wind jet which develops off the northern tip of Madagascar, whereas the poleward current weakens due to the opposing force imposed by the southwesterlies. Additionally, the circulation in the basin consist of meso-scale eddies of both polarities. Anti-cyclonic eddies, with lifespans of 2014-08-13T19:48:42Z 2014-08-13T19:48:42Z 2013 Doctoral Thesis Doctoral Ph D http://hdl.handle.net/11427/6467 eng application/pdf Department of Oceanography Faculty of Science University of Cape Town
spellingShingle Oceanography
Collins, Charine
The dynamics and physical processes of the Comoros Basin
thesis_degree_str Doctoral
title The dynamics and physical processes of the Comoros Basin
title_full The dynamics and physical processes of the Comoros Basin
title_fullStr The dynamics and physical processes of the Comoros Basin
title_full_unstemmed The dynamics and physical processes of the Comoros Basin
title_short The dynamics and physical processes of the Comoros Basin
title_sort dynamics and physical processes of the comoros basin
topic Oceanography
url http://hdl.handle.net/11427/6467
work_keys_str_mv AT collinscharine thedynamicsandphysicalprocessesofthecomorosbasin
AT collinscharine dynamicsandphysicalprocessesofthecomorosbasin