Japan Geoscience Union Meeting 2019

Presentation information

[J] Oral

H (Human Geosciences ) » H-DS Disaster geosciences

[H-DS13] Tsunami and Tsunami Forecast

Tue. May 28, 2019 3:30 PM - 5:00 PM Convention Hall B (2F)

convener:Naotaka YAMAMOTO CHIKASADA(National Research Institute for Earth Science and Disaster Resilience), Hiroaki Tsushima(Japan Meteorological Agency), Tatsuya Kubota(National Research Institute for Earth Science and Disaster Resilience), Chairperson:Osamu Sandanbata, Tatsuya Kubota

3:45 PM - 4:00 PM

[HDS13-02] Tsunami Source of the 2018 Sulawesi Earthquake Estimated from Tsunami and InSAR Data

*Tungcheng Ho1, Kenji Satake1, Shingo Watada1, Ray Y Chuang2, Chih-Heng Lu2 (1.Earthquake Research Institute,The University of Tokyo, 2.Department of Geography, National Taiwan University)

Keywords:Palu, tsunami, InSAR, Sulawesi Earthquake, source inversion

An unexpected destructive tsunami struck Palu Bay after the Mw 7.5 strike-slip faulting earthquake in Sulawesi, Indonesia, on 28 September 2018. This tsunami impacted Palu city with 5 m to 10 m runup. The combined effects of the earthquake and tsunami caused a few thousand casualties. The tsunami waves were observed by two tide gauges in Sulawesi. One tide gauge at Pantoloan port in the bay recorded tsunami waves starting at about 5 minutes after the earthquake with amplitudes of up to 2 m. The other tide gauge at Mamuju port recorded tsunami waves after about 20 minutes with peaks of about 10 cm. To understand the mechanism of this unusual tsunami, we jointly utilized the tsunami records and InSAR data to analyze the source of this earthquake. The InSAR data observed by Sentinel-1 well resolved the offset of horizontal ground movement in the direction of the orbit azimuth along the fault strike. The data show a strike of about 358° in the north of the bay and about 352° in the south of the bay. The magnitude of the offsets varied from about 1 m in the north to up to 5 m in the south. Our simple modeling result suggests a slip of about 5 m at the north and a slip up to 8 m at the south to reproduce the observed tsunami waveform at Pantoloan. The southern asperity extended about 40 km from the bay with a width of about 16 km. Tsunami travel time analysis showed that the main tsunami arrived at the Mamuju station after about 45 minutes which means the first tsunami wave at this station was triggered by another source.