Distribution of runup heights of the December 26, 2004 tsunami in the Indian Ocean

A massive earthquake with magnitude 9.3 occurred on December 26, 2004 off the northern Sumatra generated huge tsunami waves affected many coastal countries in the Indian Ocean. A number of field surveys have been performed after this tsunami event; in particular, several surveys in the south/east co...

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Bibliographic Details
Published inGeophysical research letters Vol. 33; no. 13; pp. L13601 - n/a
Main Authors Choi, Byung Ho, Hong, Sung Jin, Pelinovsky, Efim
Format Journal Article
LanguageEnglish
Published American Geophysical Union 01.07.2006
Blackwell Publishing Ltd
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Summary:A massive earthquake with magnitude 9.3 occurred on December 26, 2004 off the northern Sumatra generated huge tsunami waves affected many coastal countries in the Indian Ocean. A number of field surveys have been performed after this tsunami event; in particular, several surveys in the south/east coast of India, Andaman and Nicobar Islands, Sri Lanka, Sumatra, Malaysia, and Thailand have been organized by the Korean Society of Coastal and Ocean Engineers from January to August 2005. Spatial distribution of the tsunami runup is used to analyze the distribution function of the wave heights on different coasts. Theoretical interpretation of this distribution is associated with random coastal bathymetry and coastline led to the log‐normal functions. Observed data also are in a very good agreement with log‐normal distribution confirming the important role of the variable ocean bathymetry in the formation of the irregular wave height distribution along the coasts.
Bibliography:ark:/67375/WNG-RXFK733G-Q
istex:89081E967C86CFCFD6EF211C3A353A20D9181437
ArticleID:2006GL025867
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ISSN:0094-8276
1944-8007
DOI:10.1029/2006GL025867