Simulating the Coastal Ocean Circulation Near the Cape Peninsula Using a Coupled Numerical Model

A coupled numerical hydrodynamic model is presented for the Cape Peninsula region of South Africa. The model is intended to support a range of interdisciplinary coastal management and research applications, given the multifaceted socio-economic and ecological value of the study area. Calibration and...

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Main Authors: Marc de Vos, Marcello Vichi, Christo Rautenbach
Format: Article
Language:English
Published: MDPI AG 2021-03-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:https://www.mdpi.com/2077-1312/9/4/359
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spelling doaj-1bc035f07ffc425ba3c0b60fe4a55de32021-03-27T00:07:20ZengMDPI AGJournal of Marine Science and Engineering2077-13122021-03-01935935910.3390/jmse9040359Simulating the Coastal Ocean Circulation Near the Cape Peninsula Using a Coupled Numerical ModelMarc de Vos0Marcello Vichi1Christo Rautenbach2Marine Research Unit, South African Weather Service, Cape Town 7525, South AfricaDepartment of Oceanography, University of Cape Town, Rondebosch 7701, South AfricaDepartment of Oceanography, University of Cape Town, Rondebosch 7701, South AfricaA coupled numerical hydrodynamic model is presented for the Cape Peninsula region of South Africa. The model is intended to support a range of interdisciplinary coastal management and research applications, given the multifaceted socio-economic and ecological value of the study area. Calibration and validation are presented, with the model reproducing the mean circulation well. Maximum differences between modelled and measured mean surface current speeds and directions of 3.9 × 10<sup>−2 </sup>m s<sup>−1 </sup>and 20.7°, respectively, were produced near Cape Town, where current velocities are moderate. At other measurement sites, the model closely reproduces mean surface and near-bed current speeds and directions and outperforms a global model. In simulating sub-daily velocity variability, the model’s skill is moderate, and similar to that of a global model, where comparison is possible. It offers the distinct advantage of producing information where the global model cannot, however. Validation for temperature and salinity is provided, indicating promising performance. The model produces a range of expected dynamical features for the domain including upwelling and vertical current shear. Nuances in circulation patterns are revealed; specifically, the development of rotational flow patterns within False Bay is qualified and an eddy in Table Bay is identified.https://www.mdpi.com/2077-1312/9/4/359Cape PeninsulaTable BayFalse Bayhydrodynamic modellingcoastal currentswaves
collection DOAJ
language English
format Article
sources DOAJ
author Marc de Vos
Marcello Vichi
Christo Rautenbach
spellingShingle Marc de Vos
Marcello Vichi
Christo Rautenbach
Simulating the Coastal Ocean Circulation Near the Cape Peninsula Using a Coupled Numerical Model
Journal of Marine Science and Engineering
Cape Peninsula
Table Bay
False Bay
hydrodynamic modelling
coastal currents
waves
author_facet Marc de Vos
Marcello Vichi
Christo Rautenbach
author_sort Marc de Vos
title Simulating the Coastal Ocean Circulation Near the Cape Peninsula Using a Coupled Numerical Model
title_short Simulating the Coastal Ocean Circulation Near the Cape Peninsula Using a Coupled Numerical Model
title_full Simulating the Coastal Ocean Circulation Near the Cape Peninsula Using a Coupled Numerical Model
title_fullStr Simulating the Coastal Ocean Circulation Near the Cape Peninsula Using a Coupled Numerical Model
title_full_unstemmed Simulating the Coastal Ocean Circulation Near the Cape Peninsula Using a Coupled Numerical Model
title_sort simulating the coastal ocean circulation near the cape peninsula using a coupled numerical model
publisher MDPI AG
series Journal of Marine Science and Engineering
issn 2077-1312
publishDate 2021-03-01
description A coupled numerical hydrodynamic model is presented for the Cape Peninsula region of South Africa. The model is intended to support a range of interdisciplinary coastal management and research applications, given the multifaceted socio-economic and ecological value of the study area. Calibration and validation are presented, with the model reproducing the mean circulation well. Maximum differences between modelled and measured mean surface current speeds and directions of 3.9 × 10<sup>−2 </sup>m s<sup>−1 </sup>and 20.7°, respectively, were produced near Cape Town, where current velocities are moderate. At other measurement sites, the model closely reproduces mean surface and near-bed current speeds and directions and outperforms a global model. In simulating sub-daily velocity variability, the model’s skill is moderate, and similar to that of a global model, where comparison is possible. It offers the distinct advantage of producing information where the global model cannot, however. Validation for temperature and salinity is provided, indicating promising performance. The model produces a range of expected dynamical features for the domain including upwelling and vertical current shear. Nuances in circulation patterns are revealed; specifically, the development of rotational flow patterns within False Bay is qualified and an eddy in Table Bay is identified.
topic Cape Peninsula
Table Bay
False Bay
hydrodynamic modelling
coastal currents
waves
url https://www.mdpi.com/2077-1312/9/4/359
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