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
相关论文
共 171 条
  • [11] Irazoqui Apecechea M(2018)Operation Phakisa and unlocking South Africa ’s ocean economy J Indian Ocean Region 34 3604-3615
  • [12] de Moel H(2014)A 66-year tropical cyclone record for South-East Africa: temporal trends in a global context Int J Climatol 17 1129-1154
  • [13] Ward PJ(1997)Simulations by the atmospheric model intercomparison project of atmospheric circulation over Southern Africa Int J Climatol 77 437-471
  • [14] Aerts JCJH(1996)The NCEP/NCAR 40-Year reanalysis project Bull Am Meteor Soc 14 1271-1285
  • [15] Brown JM(2007)Ocean current and wave effects on wind stress drag coefficient over the global ocean Geophys Res Lett 11 324-336
  • [16] Souza AJ(1984)On the existence of a fully developed wind-sea spectrum J Phys Oceanogr 97 119-130
  • [17] Wolf J(1981)Open ocean momentum flux measurements in moderate to strong winds J Phys Oceanogr 4 237-259
  • [18] Brown A(2001)The oceans around southern Africa and regional effects of global change S Afr J Sci 130 725-738
  • [19] Milton S(2012)A Perspective on sea level rise and coastal storm surge from southern and eastern Africa: a case study near Durban, south Africa Water (Switzerland) 7 11969-101
  • [20] Cullen M(2004)A study of departures from the inverse-barometer response of sea level to air-pressure forcing at a period of 5 days Q J R Meteorol Soc 14 81-629