source: production/onslow_2006/report/tsunami_scenario.tex @ 3157

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1The tsunamigenic event used for this study was developed for a
2preliminary tsunami hazard assessment study delivered to FESA in September 2005,
3\cite{BC:FESA}. In that assessment, a suite of Mw 9 earthquakes
4were evenly spaced along the Sunda Arc subduction zone and there
5was no consideration of likelihood. Other sources were not considered, such
6as intra-plate earthquakes near the WA coast, volcanoes, landslides
7or asteroids. The preliminary assessment argued
8that the maximum magnitude of earthquakes off Java is at least 8.5 and
9could potentially be as high as 9.
10
11Current studies underway in GA are building probabilistic
12models to develop a more complete tsunami hazard assessment
13for the Sunda Arc subduction zone,
14due for completion in late 2006. In the preliminary assessment for
15example, it was argued that while Mw 7 and 8 earthquakes are expected
16to occur with a greater frequency than Mw 9 events,
17they are likely to pose a comparatively low and more localised hazard to WA.
18
19FESA are interested in the ``most frequent worst case scenario''. Whilst
20we cannot determine what that event may be, the Mw 9 event provides
21a plausible worst case scenario.
22
23Figure \ref{fig:mw9} shows the maximum wave height up to the 50m contour
24for a Mw 9 event off
25the coast of Java. It is this event which provides the source and
26boundary condition to the
27inundation modelling presented in this report. Description of the boundary
28condition particular to the Onslow study area
29follows in Section \ref{sec:anuga}.
30
31
32\begin{figure}[hbt]
33
34  \centerline{ \includegraphics[width=100mm, height=75mm]
35{../report_figures/mw9.jpg}}
36
37  \caption{Maximum wave height (in cms) for a Mw 9 event off the
38coast of Java}
39  \label{fig:mw9}
40\end{figure}
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