Fig. 11
From: Stochastic ground motion simulation of the 2016 Meinong, Taiwan earthquake
Distribution of residuals for each station of four models. Warm tones indicate overestimation of PGA, while cool tones indicate underestimation of PGA. a The stochastic model without site correction, b the site-corrected stochastic model using the weak events HVSR, c the site-corrected stochastic model using the mainshock HVSR, demonstrating the northwestward rupture directivity and the division of forward and backward rupture directivity, d the GMPE model by Jean et al. (2006) and Chang et al. (2010)