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IUGG XXIV General Assembly July 2-13, 2007 Perugia, Italy<br />

(S) - <strong>IASPEI</strong> - International Association of Seismology and Physics of the Earth's<br />

Interior<br />

JSS002 Oral Presentation 1765<br />

Supplementary Post-Tsunami Survey of 2004 Indian Ocean Tsunami in<br />

Sumatra Island and the database<br />

Prof. Koji Fujima<br />

Dept. of Civil and Environmental Eng. National Defense Academy<br />

Indian Ocean Tsunami, occurred on 26 December 2004, caused heavy damages in many countries in<br />

Indian Ocean. After the tsunami, many field investigations were performed to measure the tsunamitrace<br />

height, to examine the damage situation, and to make a suggestion for recovery planning.<br />

However, in Indonesia, the surveys with measurement were concentrated in Banda Aceh city and<br />

northwest part of Sumatra, north of latitude 5.4 degrees N (Lho-nga and Leopung), although the<br />

epicenter was estimated as 3.4 degree N. Therefore, 13 experts organized the survey team and carried<br />

out the supplementary post-tsunami survey from Leopung to Meulaboh, latitude 4.1 degrees N, through<br />

29 July to 6 August, 2006. The length of survey area is 180 km and the number of survey point is about<br />

30. The measured runup height between Leopung and Calang, 100 km south of Banda Aceh, was 13 to<br />

20 m, and the inundation height was 8 to 10 m. As a reference, runup height from Lho-nga and<br />

Leopung (13km length) was 20 to 30 m and the inundation height was 12 to 20 m. Because the lowlying<br />

land lies between Calang and Meulaboh, it was impossible to measure the runup height. However,<br />

the measured inundation height was 3 to 5.5 m, thus the runup height might become round 10 m if<br />

there was a hill in this region. The present survey shows the tsunami height distribution along the<br />

northwest coast of Sumatra. In the present survey area, many big bridges were destroyed by the<br />

tsunami. On the contrary, there were the small bridges which were left without destruction. In addition,<br />

beach erosion is severe between Calang to Meulaboh, the coastline moved over 100 m landward at the<br />

maximum. The mechanism of bridge destruction and beach erosion should be investigated for tsunami<br />

disaster reduction. The database of measurement data of Indian Ocean tsunami was established<br />

including the present data.<br />

Keywords: tsunami, survey, sumatra

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