摘要：Tsunami heights greater than 4 m were observed at several coastal tide-gauge stations during the tsunami generated by the 2011 off the Pacific coast of Tohoku Earthquake ( M w 9.0), causing thousands of casualties and damaging infrastructure along the Pacific coast of Japan.We retrospectively applied an algorithm of near-field tsunami forecasting to tsunami data that were recorded at various offshore tsunami stations 5–10 min before the tsunami reached the coastal tide-gauge stations nearest to its source.We inverted the waveform data recorded offshore to estimate the distribution of the initial sea-surface height, and then tsunami waveforms were synthesized from the estimated source to forecast tsunami arrival times and amplitudes at coastal tide-gauge stations.As a result of a retrospective application made 20 min after the earthquake, tsunamis with heights of 6–14 m were forecasted at tide-gauge stations nearest to the source where the sea-level increase due to the actual tsunami began to exceed 1 m after an elapsed time of 25 min.The result suggests a possibility that the forecasting method we used could contribute to the issuing of reliable near-field tsunami warning for M w 9 earthquakes. Key words Near-field tsunami forecasting ocean-bottom pressure gauge GPS buoy tsunami waveform inversion.
