Objective
Objective
Objective
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Estimation of the Distribution of<br />
JMA Seismic Intensity<br />
Deconvolution of surface ground motions to (outcrop) base<br />
Soil Classification (Yamazaki et al., 2000)<br />
I<br />
bi<br />
=<br />
I<br />
si<br />
−<br />
ARI<br />
i<br />
ARI: amplification of<br />
JMA Seismic<br />
Intensity based on soil<br />
classification<br />
Estimation of the Distribution of<br />
JMA Seismic Intensity<br />
Kriging interpolation at base rock<br />
Attenuation Relation (Trend Component)<br />
Attenuation Relationship<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
I = 9.014<br />
−1.89 log10 r − 0. 0085r<br />
<br />
<br />
<br />
<br />
<br />
<br />
Residual Component<br />
X<br />
Ii<br />
=<br />
I<br />
bi<br />
−<br />
I<br />
mi<br />
Interpolated by Kriging<br />
Technique
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