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Tsunami Science Four Years After the 2004 Indian Ocean Tsunami: Part II: Observation and Data Analysis - Couverture souple
Synopsis
This volume features select papers from the International Union of Geodesy and Geophysics XXIV General Assembly, held July 2007 as well as other contributions from leading scientists. The papers focus on understanding tsunami and mitigating their hazard.
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Présentation de l'éditeur
This volume features select papers from the International Union of Geodesy and Geophysics XXIV General Assembly, held July 2007 as well as other contributions from leading scientists. The papers focus on understanding tsunami and mitigating their hazard.
Les informations fournies dans la section « A propos du livre » peuvent faire référence à une autre édition de ce titre.
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Tsunami Science Four Years After the 2004 Indian Ocean Tsunami : Observation and Data Analysis
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Tsunami Science Four Years After the 2004 Indian Ocean Tsunami: Part II: Observation and Data Analysis (Pageoph Topical Volumes)
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Tsunami Science Four Years After the 2004 Indian Ocean Tsunami (Paperback)
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Birkhauser Verlag AG, Basel, 2009
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ISBN 13 : 9783034600637
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Paperback. Etat : new. Paperback. 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 1215 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. , 2007) that occurred at 0:58:53 GMT, 7:58:53 LT (USGS) (t ). The earthquake was responsible for a sudden fault slip estimated on average from 1215 m (SYNOLAKIS et al. , 2005) to 20 m (FU and SUN, 30 2006). The last two movies were analyzed in detail in order to calculate the tsunami velocity (FRITZ et al. Shipping may be from multiple locations in the US or from the UK, depending on stock availability. N° de réf. du vendeur 9783034600637
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Tsunami Science Four Years After the 2004 Indian Ocean Tsunami : Observation and Data Analysis
Edité par
Birkhäuser, 2009
ISBN 10 : 3034600631
ISBN 13 : 9783034600637
Ancien ou d'occasion
Couverture souple
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Tsunami Science Four Years After the 2004 Indian Ocean Tsunami: Part II: Observation and Data Analysis (Pageoph Topical Volumes)
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Tsunami Science Four Years After the 2004 Indian Ocean Tsunami : Part II: Observation and Data Analysis
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Tsunami Science Four Years After the 2004 Indian Ocean Tsunami : Observation and Data Analysis
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Tsunami Science Four Years After the 2004 Indian Ocean Tsunami
Edité par
Birkhäuser Basel Apr 2009, 2009
ISBN 10 : 3034600631
ISBN 13 : 9783034600637
Neuf
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Taschenbuch. Etat : Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -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. 332 pp. Englisch. N° de réf. du vendeur 9783034600637
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Tsunami Science Four Years After the 2004 Indian Ocean Tsunami, Part II
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Tsunami Science Four Years After the 2004 Indian Ocean Tsunami : Observation and Data Analysis
Edité par
Birkhäuser, 2009
ISBN 10 : 3034600631
ISBN 13 : 9783034600637
Ancien ou d'occasion
Couverture souple
Vendeur : GreatBookPricesUK, Woodford Green, Royaume-Uni
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Etat : As New. Unread book in perfect condition. N° de réf. du vendeur 6166310
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