Abstract
The eruption and collapse of the Anak Krakatau volcano generated tsunamis in the Sunda Strait on December 22, 2018, leading to damage and casualties. In this paper, we use the two-layer model and nonlinear shallow equation model to study the triggering mechanism of the tsunami event. We first simulate the tsunami generated by volcano eruption and landslide, respectively. The tsunami source is analyzed by comparing with gauge measurements. It indicates that the volume of partial collapse for the landslide is 0.2–0.3 km3. The comparison between the numerical results of landslide and tide gauge measurements presents well-fitted results, especially for the leading tsunami waves and arrival time. Computed maximum tsunami amplitude distribution points out that the most hazardous area is located at the south of the Sunda Strait (Pandeglang), which suffered the most casualties.
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Acknowledegements
This study is supported by the National Key Research and Development Program of China (Grant No. 2018YFC1407000). This work was partially supported by JSPS funding KAKENHI 19J20293 (YW). We thank the Scripps Institution of Oceanography, University of California San Diego, for the bathymetry data of the ocean floor at 30 arcsec resolution (SRTM30_Plus) and 30 meters resolution (STRM DEM) (Becker et al. 2009; available at https://opentopography.org). We thank the Geospatial Information Agency of Indonesia (Badan Informasi Geospasial; BIG) for providing the tsunami record of tide gauges. We also thank Prof. Fukashi Maeno at Earthquake Research Institute for his suggestions regarding the simulation of volcanic tsunamis. The discussion with Prof. Hua Liu and associate professor Chao An at Shanghai Jiao Tong University, and Prof. Haijiang Liu at Zhejiang University are appreciated. All authors have read and approved the final manuscript.
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Ren, Z., Wang, Y., Wang, P. et al. Numerical study of the triggering mechanism of the 2018 Anak Krakatau tsunami: eruption or collapsed landslide?. Nat Hazards 102, 1–13 (2020). https://doi.org/10.1007/s11069-020-03907-y
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DOI: https://doi.org/10.1007/s11069-020-03907-y