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a Distribution of maximum tensile strain.
b The distribution of maximum water elevations at Domain B. c The distribution of maximum water elevations in Domain C.
The distribution of maximum shear strain has clear spatial characteristics (Fig. 2(b)).
Figure 8 Distribution of maximum tsunami heights along the Pacific Coast of Shikoku.
Fig. 3 Radial distribution of maximum dust density (rho _{d, text{ max }}).
Open image in new window Fig. 9 Distribution of maximum drift response (Y-direction).
Figure 9 Distribution of maximum tsunami heights along the Pacific Coast of Kinki.
Fig. 5 Distribution of maximum shear strain rate on Kyushu Island.
Fig. 4 Monthly distribution of maximum temperature (left) and minimum temperature (right).
Figure 7 shows distribution of maximum tsunami heights along the Japanese coast for the simultaneous and delayed ruptures.
Using this method, we obtain the distribution of maximum earthquake magnitudes in future time intervals of arbitrary duration τ.
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