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JDR Vol.7 No.1 pp. 19-25
(2012)
doi: 10.20965/jdr.2012.p0019

Paper:

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Tsunami Hazard Mitigation at Palabuhanratu, Indonesia

Yuichiro Tanioka*, Hamzah Latief**,
Haris Sunendar*, Aditya Riadi Gusman*,
and Shunichi Koshimura***

*Institute of Seismology and Volcanology, Hokkaido University, N10W8 Kita-ku, Sapporo 060-0810, Japan

**Department of Oceanography, Bandung Institute of Technology, Jalan Ganesha 10, Bandung 40132, Indonesia

***Disaster Control Research Center, Graduate School of Engineering, Tohoku University, 6-6-11 Aoba, Aramaki, Aoba-ku, Sendai, 980-8579, Japan

Received:
August 1, 2011
Accepted:
December 2, 2011
Published:
January 1, 2012
Creative Commons License
Keywords:
tsunami inundation map, tsunami numerical simulation, tsunami disaster mitigation
Abstract
Several large earthquakes have recently occurred along the Sumatra-Java subduction zone, the 2004 great Sumatra-Andaman earthquake, the 2005 great Nias earthquake, the 2006 West Java tsunami earthquake, the 2007 great Bengkulu earthquake, and the 2010Mentawai tsunami earthquakes. Serious tsunami disasters were caused by the great underthrust earthquakes which ruptured the plate interface near the trench such as the 2004 Sumatra-Andaman, 2006West Java, 2010Mentawai earthquakes. At Palabuhanratu, maximum tsunami height distribution and inundation areas were computed from expected fault models located near the Java trench. The results shows that the most populated areas of Palabuhanratu would be severely damaged by the expected tsunami caused by the fault model of Mw 8.5. After discussing tsunami disaster mitigation measures with the local government, the result of tsunami inundation area in this study were used to decide tsunami evacuation areas and evacuation routes. The local government also installed tsunami evacuation sign boards near the coast.
Cite this article as:
Y. Tanioka, H. Latief, H. Sunendar, A. Gusman, and S. Koshimura, “Tsunami Hazard Mitigation at Palabuhanratu, Indonesia,” J. Disaster Res., Vol.7 No.1, pp. 19-25, 2012.
Data files:
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