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Massive landslides can generate significant tsunamis and endanger coastal communities, as shown by recent catastrophic events such as the 2018 Palu Tsunami and 2018 Sunda Strait Tsunami (e.g., Heidarzadeh et al. 2018; Takabatake et al. 2019). While a number of experimental studies have been conducted to investigate landslide generated tsunamis, most were performed using two dimensional (2D) wave flumes (e.g., Fritz et al. 2004; Takabatake et al. 2020). Thus, the present study conducted three-dimensional (3D) experiments to clarify the characteristics of landslide-generated tsunamis, and to develop empirical equations that can predict the generated wave heights and periods.Referencias
Fritz et al. (2004): Near Field Characteristics of Landslide Generated Impulse Waves. J. Waterw. Port Coast. Ocean Eng., vol. 130(6), pp. 287–302.
Heidarzadeh et al. (2018): Insights on the Source of the 28 September 2018 Sulawesi Tsunami, Indonesia Based on Spectral Analyses and Numerical Simulations. Pure Appl. Geophys. , vol. 176, pp. 25-43.
Takabatake et al. (2019): Field Survey and Evacuation Behaviour during the 2018 Sunda Strait Tsunami. Coast. Eng. J. , vol.61(4), pp. 423–443.
Takabatake et al. (2020): Physical Modeling of Tsunamis Generated by Subaerial, Partially Submerged, and Submarine Landslides. Coast. Eng. J., vol. 62(4), pp. 582– 601.
Takabatake et al. (2022): Three-Dimensional Physical Modelling of Tsunamis Generated by Partially Submerged Landslides. J. Geophys. Res. Oceans, e2021JC017826.
Esta obra está bajo una licencia internacional Creative Commons Atribución 4.0.
Derechos de autor 2023 Tomoyuki Takabatake, Dawn Chenxi Han, Miguel Esteban, Tomoya Shibayama