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The maximum tsunami run-up height, in the study area, reached 15 m at Pakarang Cape (Siripong, 2006).
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The slip amounts of 10 m and 15 m generate maximum tsunami run-ups that are close to the observation of 14 m.
The simulated tsunami run-up from the fault model is very close to the measured run-up.
Preliminary surveys reported tsunami run-up heights exceeding 30 m (The 2011 Tohoku Earthquake Tsunami Joint Survey Group, 2011).
This study proposes a method to measure geographical risk from tsunami run-up events based on socioeconomic-environmental data.
This indicates that tsunami run-up heights can be estimated from sand deposit distribution data.
The observed tsunami run-up heights were modest and typically in the range of 1 3 m.
Surprisingly, they have not been demonstrated to provide more accurate run-up predictions for tsunami run-up even for landslide waves (Lynett et al., 2003).
The simulated tsunami run-up of 12 m is close to the measured run-up from the deposition limit at elevation of 14 m.
Onshore tsunami deposits and satellite images, which show large amounts of sediment transported offshore, indicate that the seafloor was impacted by tsunami run-up and backwash.
Boundary conditions for tsunami run-up computation are determined by the judgment of a cell for being submerged or dry.
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