Figure 10From: Sensitivity of tsunami wave profiles and inundation simulations to earthquake slip and fault geometry for the 2011 Tohoku earthquakeVariability of tsunami inundation heights along the coast for the Satake et al. model. The variability is due to strike variations (a), dip variations (b), and slip variations (c). The observed inundation heights (Tohoku Tsunami Joint Survey (TTJS) results) are marked by yellow circles.Back to article page