“…These large tsunamis were clearly observed at offshore tsunami observation stations around Japan, such as cabled ocean-bottom pressure gauges (OBPGs) (e.g., Meteorological Research Institute, 1980) and GPS buoys (e.g., Kato et al, 2005), as well as by the worldwide Deepocean Assessment and Reporting of Tsunamis (DART) buoy systems (e.g., Titov et al, 2005). Because tsunamis can be detected at offshore stations earlier than at the coast, several methods of tsunami forecasting based on offshore tsunami data have been proposed for near-field tsunamis (e.g., Baba et al, 2004;Takayama, 2008;Tatsumi and Tomita, 2009;Hayashi, 2010), as well as for far-field tsunamis (Titov et al, 2005).…”