Resumen
Numerical modelling of storm tide within Moreton Bay has consistently underestimated peak tide gauge level observations by up to 40 percent during extreme events. This study tests "missing" contribution hypotheses by undertaking a series of integrated hydrodynamic and spectral wave modelling experiments, supported by high quality gridded wind, observed water level and wave data at sites throughout Moreton Bay and the Southeast Queensland coast. The case studies are the regional surge responses during the passages of Ex. Tropical Cyclone Oswald, Ex. Tropical Cyclone Debbie and Tropical Cyclone Oma. Testing of these hypotheses will contribute to an improved understanding of the key processes required to model storm surge accurately in other similar coastal embayments.Referencias
Nielsen, Callaghan & Baldock, (2011), Downward transfer of momentum by wind-driven waves, Coastal Engineering, vol. 58, no. 12, pp. 1118–1124.
Smith (2015), Southeast Queensland Storm Tide Response to Ex. Tropical Cyclone Oswald, Engineering and Sciences Department, University of Southern Queensland.
Treloar, Taylor & Prenzler (2011), Investigation of wave induced storm surge within a large coastal embayment – Moreton Bay (Australia), Coastal Engineering Proceedings, vol. 1, no. 32.
![Creative Commons License](http://i.creativecommons.org/l/by/4.0/88x31.png)
Esta obra está bajo una licencia internacional Creative Commons Atribución 4.0.
Derechos de autor 2023 Mitchell Smith, Zachariah Couper, Ian Teakle, Daryl Metters