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b Estimated tsunami source.
Tsunami source PIN is the normal component of the first four oblique-normal segments of tsunami source PI.
Such information is useful to estimate the tsunami source model (e.g. Nanayama et al., 2003).
This is an important step towards improving the tsunami source model in future work.
The real-time data directly estimate the initial tsunami height distribution as the tsunami source.
The 2011 tsunami source area includes several segments of previous recurring large earthquakes.
We set the initial sea-surface height at time t = 0 as the tsunami source.
The tsunami source models in this study correspond to four 1755-like earthquake scenarios.
Therefore, we assumed that these offshore stations were within the tsunami source area.
Tsunami heights exceeded 4 m at coastal tide-gauge stations near the tsunami source.
This westward rupture movement could be a possible tsunami source similar to the 2004 Sumatra earthquake.
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