source: production/onslow_2006/introduction.tex @ 2863

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1
2This report is being provided to the Fire and Emergency Services Authority
3(FESA)
4as part of the Collaborative Research Agreement with Geoscience Australia.
5FESA recognises the potential vulnerability of the Western Australia
6coastline to tsunamigenic earthquakes originating from
7the Sunda Arc subduction zone. There is
8historic evidence of such events and FESA has sought to assess
9the relative risk of its urban and regional communities to the tsunami
10threat and develop detailed response plans.
11
12This report is the first in a series of studies to assess the relative
13risk to the tsunami threat. The methods, assumptions and results of a
14single tsunami source scenario is described for the Onslow area in the
15North West shelf region. The return
16period of this particular scenario is unknown, however it
17can be be classed as a plausible event. Future studies
18will present a series of scenarios for a range of return events to
19assist FESA in developing appropriate plans for a range of event impacts.
20
21The software tool, ANUGA, has been used to develop the inundation extent
22and associated water height at various points in space and time.
23ANUGA has been developed by GA and the Australian National University
24(ANU) to solve the nonlinear shallow water
25wave equation using the finite volume technique (described in [1]).
26An advantage of this technique is that the cell resolution can be changed
27according to areas of interest. ANUGA is under constant development and
28validation investigations. As such, the current results represent ongoing work
29and may change in the future.
30
31The following set of information is required input to undertake the tsunami
32impact modelling and will be discussed in following sections.
33
34\begin{itemize}
35\item onshore and offshore data
36\item initial condition
37\item boundary condition
38\end{itemize}
39
40The inundation results for the Onslow area is described in section
41\ref{sec:results}.
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