Abstract
For many practical and theoretical purposes, various types of tsunami wave models have been developed and utilized so far. Some distinction among them can be drawn based on governing equations used by the model. Shallow water equations and Boussinesq equations are probably most typical ones among others since those are computationally efficient and relatively accurate compared to 3D Navier-Stokes models. From this idea, some coupling effort between Boussinesq model and shallow water equation model have been made (e.g., Son et al. (2011)). In the present study, we couple two different types of tsunami models, i.e., nondispersive shallow water model of characteristic form(MOST ver.4) and dispersive Boussinesq model of non-characteristic form(Son and Lynett (2014)) in an attempt to improve modelling accuracy and efficiency.Recorded Presentation from the vICCE (YouTube Link): https://youtu.be/cTXybDEnfsQ
References
Dongeren, A.V. and Svendsen, I.A. (1997). Absorbing-generating boundary condition for shallow water models. Journal of Waterway, Port, Coastal, and Ocean Engineering, 123(6), pp.303-313.
Son, S., Lynett, P., Kim., D. (2011) Nested and multi-physics modeling of tsunami evolution from generation to inundation, Ocean Modelling, vol. 38, no. 1-2, p.96-113
Son, S., & Lynett, P. J. (2014). Interaction of dispersive water waves with weakly sheared currents of arbitrary profile. Coastal Engineering, 90, 64-84.
Titov, V.V., Synolakis, C.E., (1995) Modeling of breaking and nonbreaking long-wave evolution and runup using VTCS-2. J. Waterway, Port, Coastal and Ocean Eng. vol. 121(6), p. 308-316.
Titov, V.V., Synolakis, C.E., (1998) Numerical modeling of tidal wave runup. J. Waterw. Port Coastal Ocean Eng. vol.124(4), p. 157-171.
Tolkova, E. (2016). Cliffs benchmarking. arXiv preprint arXiv:1601.06486.