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The experimental diodicity is reproduced well with the numerical simulation.
The CCIR model reproduced well the propagation factor.
At Bodrum, the tsunami period is reproduced well.
The calculated potential oscillation curve reproduced well the observed one.
The numerical simulations reproduced well the experimental results.
However, for shorter periods the later surface waves are not reproduced well, while the first part (P- and S-waves) is reproduced well to some extent.
The GNSS data are also reproduced well by the constructed model (Fig. 4e).
The water balance was also reproduced well during the calibration and validation periods (PBIAS < 10%%).
The agreement between the calculated theory and experiment is excellent and reproduced well.
According to Fig. 5a, the measured reflectance values are reproduced well by the Kubelka Munk equation.
In addition, the experimentally measured magnetic properties are reproduced well by micromagnetic simulations.
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