A coupled wave, tide and storm surge operational forecasting system for South Africa: validation and physical description

被引:0
作者
Christo Rautenbach
Tania Daniels
Marc de Vos
Michael A. Barnes
机构
[1] South African Weather Service,Marine Research Unit
[2] Nelson Mandela University,Institute for Coastal and Marine Research
[3] University of Cape Town,Department of Oceanography and Marine Research Institute
[4] University of Cape Town,Climate Systems Analysis Group
[5] University of Pretoria,Department of Geography, Geoinformatics and Meteorology
来源
Natural Hazards | 2020年 / 103卷
关键词
Storm surge; Waves; Extreme events; Operational forecasting; Numerical modelling; Mid-latitude cyclones; Delft 3D; SWAN; South Africa;
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中图分类号
学科分类号
摘要
Regional storm tidal levels of the South African coastline are investigated by means of a calibrated and validated numerical model. The model was developed utilizing the shallow water hydrodynamic model, Delft3D. This model was coupled (online) with a non-stationary spectral wave model (developed in the Simulating WAves in the Nearshore (SWAN) numerical code). A local, 4.4 km version of the Unified Model was applied as atmospheric forcing for the coupled system. The models presented in this study form part of the operational marine forecasts of the South African Weather Service, Wave and Storm Surge model. The operational protocol and model calibration and validation are presented via statistical correlations with measured water levels at six South African coastal locations. The main calibration parameters and thus physical drivers were winds, atmospheric pressure and waves. The validated numerical model is used to provide an experimental physical description of South African storm surge characteristics, per coastline. The dominant driver of South African storm surge is winds associated with mid-latitude cyclones. Further novelty in the present study is the quantification of the relative contribution of extreme storm wave set-up to the South African storm surge signal. This wave set-up contributes approximately 20% of the total surge signal in the southwest, with winds contributing approximately 55%. The importance of the continental shelves is also elucidated concerning the frictional shoaling effects of the long surge wave propagation.
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页码:1407 / 1439
页数:32
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共 171 条
[21]  
Golding B(2016)A global reanalysis of storm surges and extreme sea levels Nat Commun 23 619-283
[22]  
Mitchell J(2018)Projected changes in tropical cyclones over the South West Indian Ocean under different extents of global warming Environ Res Lett 422 279-956
[23]  
Shelly A(2006)Tropical cyclone induced asymmetry of sea level surge and fall and its presentation in a storm surge model with parametric wind fields Ocean Model 150 103079-107
[24]  
Cabral P(2006)Low-frequency sea level variability and the inverted barometer effect J Atmos Ocean Technol 87 941-1966
[25]  
Augusto G(2003)Reduced drag coefficient for high wind speeds in tropical cyclones Nature 2 97-588
[26]  
Akande A(2019)Tidal characteristics of South Africa Deep Sea Res Part I 16 1948-1242
[27]  
Costa A(2006)Seasonal to Decadal Prediction of Southern African Climate and Its Links with Variability of the Atlantic Ocean Bull Am Meteor Soc 91 579-276
[28]  
Amade N(1983)Long-period coastal trapped waves off the southeast coast of Southern Africa Cont Shelf Res 15 1231-953
[29]  
Niquisse S(2003)Air-sea interaction and the seasonal cycle of the subtropical anticyclones J Clim 103 274-4
[30]  
Atumane A(1995)Extreme high sea levels around the coast of southern Africa S Afr J Sci 147 940-159