Figure 2From: Sensitivity of tsunami wave profiles and inundation simulations to earthquake slip and fault geometry for the 2011 Tohoku earthquakePower spectra and misfit functions. Two-dimensional (2D) power spectrum of the Satake et al. model (Figure 1) (a), the observed and modelled one-dimensional (1D) power spectra in the down-dip and along-strike directions (b), and the misfit functions for estimating the correlation lengths in the down-dip and along-strike directions (c). The wavenumber ranges used for the quantitative spectral analysis are shown by the black rectangle in (a) and by the broken lines in (b).Back to article page