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Example of the procedure for correction of the source factor.
We can introduce the average of seismic intensity, instead of JMA magnitude, to represent source factor S in Eq. (2).
Predictions of seismic ground motion usually consider a source factor, a path factor, and a site amplification factor.
Thus, the difference between PGVobs and PGV700exp · H involves not only the site amplification factor, but also the source factor.
In introducing the average of intensity differences as the source factor, it is no longer necessary to use earthquake pairs having the same JMA magnitude.
The difference of the average of seismic intensity is considered to be the difference of the source factor that determines the seismic intensities.
Similar(18)
Extensive CAP characterization, including use of a Semicontinuous Elements in Aerosol Sampler (SEAS), was performed, and positive matrix factorization was applied to investigate source factors.
Substituting the average of the difference of seismic intensities corresponds to an adjustment of the difference of the source factors.
As described in the text, Factor 1 is most likely an intermediate crustal source, Factors 2 and/or 3 are most likely dacitic source(s) and Factor 4 is a Nb-rich end member.
Single P source factors and combinations of factors were tested and discussed together with water movement and water management factors important for catchments dominated by drained clay soils.
Attempts to understand the variability in SEP intensities have been focused on two aspects: (1) source factors involving CME properties, (2) environmental factors such as ambient magnetosonic speed, preceding CMEs, deflection by large-scale structures, seed particles, and turbulence.
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