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Impact of Wind Driven Variability on Sea Surface Temperature and Ocean Colour in False Bay

False Bay is the largest true bay in South Africa and is an important area for conservation, the local fishing industry and marine based recreational activities. A large amount of studies, both recent and historical, have been carried out on the biology of the bay, but studies on the physics of the...

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Main Author: Seymour, Sian
Other Authors: Krug, Marjolaine
Format: Thesis
Language:English
Published: Department of Oceanography 2020
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access_status_str Open Access
author Seymour, Sian
author2 Krug, Marjolaine
author_browse Krug, Marjolaine
Seymour, Sian
author_facet Krug, Marjolaine
Seymour, Sian
author_sort Seymour, Sian
collection Thesis
description False Bay is the largest true bay in South Africa and is an important area for conservation, the local fishing industry and marine based recreational activities. A large amount of studies, both recent and historical, have been carried out on the biology of the bay, but studies on the physics of the bay are very few in comparison. In this study high resolution satellite imagery is used to investigate wind variability and its impact on sea surface temperature (SST) and chlorophyll concentration (Chl-a) variability within False Bay and the Cape Peninsula region. High resolution (1 km) coastal winds derived from the Sentinel-1 satellite Synthetic Aperture Radar (SAR) show that winds are strongly influenced by topography under the predominantly south-easterly wind regime. The Hottentots Holland mountain range and Cape Peninsula mountain range create wind shadows as well as areas of increased wind speed within False Bay and west of the Cape Peninsula. Our observations also show that global atmospheric models, such as ECMWF, are not able to capture the spatial variability in the wind fields driven by the orography. Analyses of the SST and ocean colour imagery show that wind shadows are generally associated with warmer surface waters and higher Chl-a. In contrast, regions of enhanced wind speeds show colder surface waters and decreased chlorophyll concentration. Our results suggest that spatial variation in the horizontal wind fields have direct and significant impact on the water properties within False Bay. This study highlights the need for high resolution wind observations and simulations to force regional oceanic models of False Bay and the Cape Peninsula region.
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institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:32:05.102Z
license_str Not specified — see source repository
provenance_str_mv Harvested via OAI-PMH from UCTD — University of Cape Town Open Access Repository
publishDate 2020
publishDateRange 2020
publishDateSort 2020
publisher Department of Oceanography
publisherStr Department of Oceanography
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source_str UCTD — University of Cape Town Open Access Repository
spelling oai:open.uct.ac.za:11427/31235 Impact of Wind Driven Variability on Sea Surface Temperature and Ocean Colour in False Bay Seymour, Sian Krug, Marjolaine Smith, Marie Mouche, Alexis Rouault, Mathieu Applied Ocean Sciences False Bay is the largest true bay in South Africa and is an important area for conservation, the local fishing industry and marine based recreational activities. A large amount of studies, both recent and historical, have been carried out on the biology of the bay, but studies on the physics of the bay are very few in comparison. In this study high resolution satellite imagery is used to investigate wind variability and its impact on sea surface temperature (SST) and chlorophyll concentration (Chl-a) variability within False Bay and the Cape Peninsula region. High resolution (1 km) coastal winds derived from the Sentinel-1 satellite Synthetic Aperture Radar (SAR) show that winds are strongly influenced by topography under the predominantly south-easterly wind regime. The Hottentots Holland mountain range and Cape Peninsula mountain range create wind shadows as well as areas of increased wind speed within False Bay and west of the Cape Peninsula. Our observations also show that global atmospheric models, such as ECMWF, are not able to capture the spatial variability in the wind fields driven by the orography. Analyses of the SST and ocean colour imagery show that wind shadows are generally associated with warmer surface waters and higher Chl-a. In contrast, regions of enhanced wind speeds show colder surface waters and decreased chlorophyll concentration. Our results suggest that spatial variation in the horizontal wind fields have direct and significant impact on the water properties within False Bay. This study highlights the need for high resolution wind observations and simulations to force regional oceanic models of False Bay and the Cape Peninsula region. 2020-02-21T13:48:58Z 2020-02-21T13:48:58Z 2019 2020-02-21T09:14:53Z Master Thesis Masters MSc http://hdl.handle.net/11427/31235 eng application/pdf Department of Oceanography Faculty of Science
spellingShingle Applied Ocean Sciences
Seymour, Sian
Impact of Wind Driven Variability on Sea Surface Temperature and Ocean Colour in False Bay
thesis_degree_str Master's
title Impact of Wind Driven Variability on Sea Surface Temperature and Ocean Colour in False Bay
title_full Impact of Wind Driven Variability on Sea Surface Temperature and Ocean Colour in False Bay
title_fullStr Impact of Wind Driven Variability on Sea Surface Temperature and Ocean Colour in False Bay
title_full_unstemmed Impact of Wind Driven Variability on Sea Surface Temperature and Ocean Colour in False Bay
title_short Impact of Wind Driven Variability on Sea Surface Temperature and Ocean Colour in False Bay
title_sort impact of wind driven variability on sea surface temperature and ocean colour in false bay
topic Applied Ocean Sciences
url http://hdl.handle.net/11427/31235
work_keys_str_mv AT seymoursian impactofwinddrivenvariabilityonseasurfacetemperatureandoceancolourinfalsebay