Fig. 4.From: The 2011 Mw 9.0 off the Pacific coast of Tohoku Earthquake: Comparison of deep-water tsunami signals with finite-fault rupture model predictionsSensitivity tests of slip location for prediction of DART tsunami recordings using the P-Mod solution with the entire grid laterally shifted 40-km WNW, 20-km WNW, 20-km ESE, 40-km ESE, and 35-km E. Observed waveforms (black lines) and synthetic predictions (red lines) are shown for the stations modeled in Fig. 3.Back to article page