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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.
We used U.S. Environmental Protection Agency EPAA) Positive Matrix Factorization (PMF) 3.0 (U.S. EPA 2010) to investigate source factors; PMF is a variant of factor analysis that constrains factor loadings and factor scores to nonnegative values and has been described in detail (Paatero and Tapper 1994).
Substituting the average of the difference of seismic intensities corresponds to an adjustment of the difference of the source factors.
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.
In the expansion (21), the terms that do not include the source factors J and (tilde{J}) only contribute to the normalization (Z[0,0]) and do not affect moments because of (18).
Similar(28)
Example of the procedure for correction of the source factor.
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.
We can introduce the average of seismic intensity, instead of JMA magnitude, to represent source factor S in Eq. (2).
Even when the source factor and path factor are appropriately evaluated, we should expect errors of if the site amplification factor is represented by single scalar value.
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