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The maximum slip values for the 11 models vary significantly (from 35 to 75 m).
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(Here, the average rupture velocity of each large slip area is defined to track the onset when the slip value reaches 2 m, which is approximately 30% of the maximum slip value for slip areas B, C, and D).
Fig. 4 a Seafloor deformation from source models based on nodal planes 1 (left) and 2 (right) for slip values of 0.4 m for the 20 July 2017 Bodrum Kos tsunami.
Tsunami simulations and comparison with observed waveforms are presented in Fig. 4 for both nodal planes NP-1 and NP-2 and for the slip value of 0.4 m.
The Box-Cox parameter is relatively stable across different slip models; the logarithmic transformation case, having a heavier right tail than λ = 0.2 to 0.3, was obtained from model 11 (which has large slip values that exceed 70 m for some cells).
To equalise the characteristics of the original and synthesised slip distributions, we implemented a scaling and modification procedure for the synthesised slip values by (i) using the Box-Cox power transformation and (ii) adjusting the mean and standard deviation of the transformed slip distribution.
Then, the mean and standard deviation of the slip values are adjusted to ensure that the amount of seismic moment for the simulated slip field is similar to that for the original slip model.
For all cases, a constant peak region appeared at slip values between 5 and 10 mm.
It was also found that coefficient of variation of bond strength and corresponding slip value increased significantly for corroded members compared to that of intact members.
From bending tests, the interface slip value is evaluated.
Slip value (mm).
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