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In this simulation, we use a 500-m resolution bathymetry model constructed by combining the ETOPO1 global Earth model and the J-EGG500 Japan coastal model for tsunami computation.
Jaffe and Gelfenbuam (2007) developed a simple model for tsunami sedimentation that can be applied to calculate tsunami flow speed from the thickness and grain size of a tsunami deposit.
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Here, assuming that the tsunami is simulated using a proven numerical code that is capable of predicting tsunami propagation and inundation based on a theory for long waves, we newly modeled the spread and burning behavior of oil on water in tsunamis, and integrated the models for tsunami flow, oil spread and oil burning.
To assess the potential tsunami hazard, it is crucial to apply physically reliable earthquake models for tsunami simulation to obtain more realistic tsunamis.
These results also contribute to the construction of the seismic source fault models for tsunamis and seismic hazard estimations of this region.
We proposed a source fault model for this tsunami with the length and width of 25 and 15 km and uniform slip of 0.4 m.
To address this, he proposed a model for a tsunami warning system specific for the Marmara region that is strongly coupled with the earthquake early warning system and stakeholders of tsunami mitigation activities, such as the local and regional components of disaster and emergency management and civil protection units.
Fig. 2. (a) Computational domain for the model of tsunami propagation and run-up to Sendai Plain and ultimate sea-bottom deformation as a wave source of the Tohoku-oki tsunami (Imamura et al., 2011).
In this study, a new approach is applied to define tsunami human vulnerability parameters, and a new model for high-resolution tsunami risk analysis based on tsunami numerical modeling and GIS-based MCDA is proposed.
We also tested whether numerical modeling for the tsunami inundation can reproduce the ground truth.
Rahiman et al. ([2007]) established submarine landslide-generated surge source model and earthquake-generated tsunami model for numerical simulation of Suva Tsunami in 1953.
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