Figure 12From: Sensitivity of tsunami wave profiles and inundation simulations to earthquake slip and fault geometry for the 2011 Tohoku earthquakeVariability of tsunami wave profiles at four GPS buoys for different models. Models 1 to 6 (a) and models 7 to 11 (b). Note the overall agreement of all model predictions with the observations (black line) at long wavelengths, but the substantial variations in peak amplitude and timing (in particular at the Miyagi sites).Back to article page