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A climatology of the coastal low in the SW Cape

Bibliography: leaves 103-109.

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Bibliographic Details
Main Author: Heydenrych, Clive Malcolm
Other Authors: Keen, Cecil
Format: Thesis
Language:English
Published: Department of Environmental and Geographical Science 2015
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access_status_str Open Access
author Heydenrych, Clive Malcolm
author2 Keen, Cecil
author_browse Heydenrych, Clive Malcolm
Keen, Cecil
author_facet Keen, Cecil
Heydenrych, Clive Malcolm
author_sort Heydenrych, Clive Malcolm
collection Thesis
description Bibliography: leaves 103-109.
format Thesis
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institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:46:06.060Z
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 Environmental and Geographical Science
publisherStr Department of Environmental and Geographical Science
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source_str UCTD — University of Cape Town Open Access Repository
spelling oai:open.uct.ac.za:11427/14293 A climatology of the coastal low in the SW Cape Heydenrych, Clive Malcolm Keen, Cecil Geography and Environmental Studies Bibliography: leaves 103-109. The Coastal Low is a shallow cyclonic mesoscale weather 'disturbance' which migrates around the southern African subcontinent on a fairly regular basis. It is generated and maintained by the synoptic scale circulations. The movement and surface characteristics have been well documented by a number of authors but few detailed studies have been undertaken on its vertical structure in southern Africa. In addition to this, most of the previous work has been of a meteorological nature. This study has concentrated on a more climatic approach in its investigation of the vertical and· surface features of the Coastal Low as it migrates through the South Western (SW) Cape. The SW Cape is a 'transition region' for the migration of the Coastal Low; situated between the west and south coasts with a distinct local climate due to the complex topography of the region. This fact tends to alter the characteristic features of the Coastal Low system but appears not to prevent the Coastal Low from migrating through the region. The Coastal Low is regarded as being an internal trapped Kelvin wave and corrected surface pressure values best indicate its migration characteristics. However upper air analysis indicates that temperature values (between 950- 900mb) at the level of the inversion, produce one of the best signatures of the Coastal Low's passage. This is related to the strong subsidence from above the 850mb level in the pre-Low period. This strong divergence dynamically compresses the lower layers into low level wind speed maxima on either side of the centre of the system. The Coastal Low appears to have a very complex structure, and two results from this study in the. SW Cape bear particular mention. Firstly the offshore flow at the escarpment level is weakly defined. Secondly also, the longshore spatial extent of the Coastal Low system has been estimated to have an 'inner' diameter of 150-200km and an 'outer' diameter of approximately 1000km. 2015-10-25T16:59:42Z 2015-10-25T16:59:42Z 1987 Master Thesis Masters MSc http://hdl.handle.net/11427/14293 eng application/pdf Department of Environmental and Geographical Science Faculty of Science University of Cape Town
spellingShingle Geography and Environmental Studies
Heydenrych, Clive Malcolm
A climatology of the coastal low in the SW Cape
thesis_degree_str Master's
title A climatology of the coastal low in the SW Cape
title_full A climatology of the coastal low in the SW Cape
title_fullStr A climatology of the coastal low in the SW Cape
title_full_unstemmed A climatology of the coastal low in the SW Cape
title_short A climatology of the coastal low in the SW Cape
title_sort climatology of the coastal low in the sw cape
topic Geography and Environmental Studies
url http://hdl.handle.net/11427/14293
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