Although only about 5% of tsunamis have been generated by volcanic eruptions, these tsunamis caused approximately 25% of all the deaths associated with volcanic eruptions (Latter, 1981;Mastin & Witter, 2000). Compared with tsunamis generated by subaerial volcanic eruptions, tsunamis generated by submarine volcanic eruptions are more complicated and less studied by researchers. This is because a number of poorly understood processes combine to produce sudden and dynamic effects. First, the source properties of submarine volcanic eruptions are still poorly understood (White et al., 2015) despite direct observations of the