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Tsunami Science Four Years After the 2004 Indian Ocean Tsunami - Part II: Observation and Data Analysis (Paperback, 2009 ed.)
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Tsunami Science Four Years After the 2004 Indian Ocean Tsunami - Part II: Observation and Data Analysis (Paperback, 2009 ed.)
Series: Pageoph Topical Volumes
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The 2004 Indian Ocean tsunami was triggered by a 9. 15 magnitude
earthquake (MELTZNER et al. , 2006; CHLIEH et al. , 2007) that
occurred at 0:58:53 GMT, 7:58:53 LT (USGS) (t ). The epicenter was
located at 3. 3 N, 95. 8 E (Fig. 1) with a focal depth of EQ
approximately 30 km. The earthquake was responsible for a sudden
fault slip estimated on average from 12-15 m (SYNOLAKIS et al. ,
2005; LAY et al. , 2005) to 20 m (FU and SUN, 30 2006). The seismic
moment estimate (Mo = 1. 3 5 9 10 dyne-cm), based on the Figure 1
Locations of video recordings, recovered clocks, and reliable
eyewitness observations. 1: Coastal plains ?ooded by the tsunami;
2: non-?ooded coastal plains; 3: uplands. Insert 3D-map showing the
Sumatra Island, the studied area, and the epicenter of the
26/12/2004 earthquake. The video taken at Uteuen Badeue, on the
eastern edge of the Banda Aceh Bay, was recorded by the chief of
the Fishery Regional Of?ce from the top of a cliff. The movie that
was shot near the Baiturrahman mosque in downtown Banda Aceh has
been shown worldwide on TV. The one at Peukan Bada has been
recorded during a wedding party. The last two movies were analyzed
in detail in order to calculate the tsunami velocity (FRITZ et al.
, 2006). Vol.
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