“…The coseismic slip of the Tohoku‐oki earthquake was estimated from seismic waveform data (Ammon et al., 2011; Hayes, 2011; Ide et al., 2011; Satriano et al., 2014; Shao et al., 2011; Suzuki et al., 2011; Uchide, 2013; Yagi & Fukahata, 2011; Yoshida et al., 2011), geodetic surface deformation measurements (Iinuma et al., 2012; Ito, et al., 2011; Kyriakopoulos et al., 2013; Ozawa et al., 2012; Perfettini & Avouac, 2014; Pollitz et al., 2011; Silverii et al., 2014; Zhou et al., 2014), high‐rate GPS time series (Wang et al., 2016; Yue & Lay, 2011), tsunami wave observations (Fujii et al., 2011; Hossen et al., 2015; Maeda et al., 2011; Saito et al., 2011; Satake et al., 2013), InSAR, and various combinations of these data (Bletery et al., 2014; Gusman et al., 2012; Hooper et al., 2013; Koketsu et al., 2011; Kubo & Kakehi, 2013; Lee et al., 2011; Melgar & Bock, 2015; Minson et al., 2014; Romano et al., 2012, 2014; Wang et al., 2012; Wang et al., 2013; Wei et al., 2012; Yamazaki et al., 2018; Yokota et al., 2011; Yue & Lay, 2013) (Figure 12). Resolution tests of models constrained by individual datasets indicate that the strong motion data alone have limited resolution of slip updip from the hypocenter, while inversions of on‐land static geodetic data can resolve slip out to the hypocenter but have no resolution of slip near the trench (Wei et al., 2012).…”