When is a tsunami a mega-tsunami?
dc.contributor.author | Chagué-Goff, C | en_AU |
dc.contributor.author | Goff, JR | en_AU |
dc.contributor.author | Terry, JP | en_AU |
dc.contributor.author | Goto, K | en_AU |
dc.date.accessioned | 2017-04-12T23:56:26Z | en_AU |
dc.date.available | 2017-04-12T23:56:26Z | en_AU |
dc.date.issued | 2014-01-12 | en_AU |
dc.date.statistics | 2017-04-11 | en_AU |
dc.description.abstract | The 2004 Indian Ocean Tsunami is commonly called a mega-tsunami, and this attribute has also been linked to the 2011 Tohoku-oki tsunami. However, since this term was first coined in the early 1990's there have been very few attempts to define it. As such it has been applied in a rather arbitrary fashion to a number of tsunami characteristics, such as wave height or amplitude at both the source and at distant locations, run-up height, geographical extent and impact. The first use of the term is related to a tsunami generated by a large bolide impact and indeed it seems entirely appropriate that the term should be used for such rare events on geological timescales. However, probably as a result of media-driven hyperbole, scientists have used this term at least twice in the last decade, which is hardly a significant portion of the geological timescale. It therefore seems reasonable to suggest that these recent unexpectedly large events do not fall in the category of mega-tsunami but into a category of exceptional events within historical experience and local perspective. The use of the term mega-tsunami over the past 14 years is discussed and a definition is provided that marks the relative uniqueness of these events and a new term, appropriately Japanese in origin, namely that of souteigai-tsunami, is proposed. Examples of these tsunamis will be provided. | en_AU |
dc.identifier.citation | Chagué-Goff, C., Goff, J., Terry, J. P., & Goto, K. (2014). When is a tsunami a mega-tsunami? Paper presented at the AGU Fall Meeting 15-19 December 2014, San Francisco, America. | en_AU |
dc.identifier.conferenceenddate | 19 December 2014 | en_AU |
dc.identifier.conferencename | AGU Fall Meeting | en_AU |
dc.identifier.conferenceplace | San Francisco, America | en_AU |
dc.identifier.conferencestartdate | 15 December 2014 | en_AU |
dc.identifier.govdoc | 8091 | en_AU |
dc.identifier.issn | NH21A-3827 | en_AU |
dc.identifier.uri | https://agu.confex.com/agu/fm14/meetingapp.cgi/Paper/21677 | en_AU |
dc.identifier.uri | http://apo.ansto.gov.au/dspace/handle/10238/8557 | en_AU |
dc.language.iso | en | en_AU |
dc.publisher | American Geophysical Union | en_AU |
dc.subject | Seas | en_AU |
dc.subject | Tsunamis | en_AU |
dc.subject | Geology | en_AU |
dc.subject | Impact strength | en_AU |
dc.subject | Japan | en_AU |
dc.subject | Geology | en_AU |
dc.title | When is a tsunami a mega-tsunami? | en_AU |
dc.type | Conference Abstract | en_AU |
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