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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 1769<br />

A Probabilistic Tsunami Hazard Assessment for Western Australia<br />

Dr. Phil Cummins<br />

Geospatial and Earth Monitoring Division Geoscience Australia <strong>IASPEI</strong><br />

David Burbidge, Hong Kie Thio<br />

The occurrence of the Indian Ocean Tsunami on 26 December, 2004 has raised concern about the lack<br />

of information on the tsunami threat, which makes it difficult to determine appropriate mitigation<br />

measures. In addition to a warning system, such measures may include inundation maps and decisionmaking<br />

tools that would enable planning and emergency management officials to manage the tsunami<br />

threat. A first step in the development of such measures is a tsunami hazard assessment, which gives<br />

an indication of which areas of coastline are most likely to experience tsunami, and how likely such<br />

events are. Here we present the results of a probabilistic tsunami hazard assessment for Western<br />

Australia (WA). Compared to other parts of Australia, the WA coastline experiences a a relatively higher<br />

frequency of tsunami occurrence. This hazard is due to earthquakes along the Sunda Arc, south of<br />

Indonesia. Our work shows that large earthquakes offshore of Java and Sumba are likely to be a greater<br />

threat to WA than those offshore of Sumatra or elsewhere in Indonesia. A magnitude 9 earthquake<br />

offshore of the Indonesian islands of Java or Sumba has the potential to significantly impact a large part<br />

of the West Australian coastline. The level of hazard varies along the coast, but is highest along the<br />

coast from Carnarvon to Dampier. Tsunami generated by other sources (e.g. large intra-plate events,<br />

volcanoes, landslides and asteroids) were not considered in this study, which limits our hazard<br />

assessment to recurrence times of 2000 years or less.<br />

Keywords: tsunami, hazard, modelling

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