“…The reasons include dissimilar fundamental frequencies of the participating structural members, spatially varying ground motion, and soil-structure interaction (SSI) (Chouw and Hao, 2009;Raheem, 2009;Bi et al, 2010Bi et al, , 2011. Spatial variation of ground motion arises mainly from three sources, i.e., the wave passage effect arising from finite wave velocity, loss of coherency because of reflection, refraction, and superposition of the seismic waves and the site effect resulting from different local soil conditions (Kiureghian and Neuenhofer, 1992).…”