source: production/pt_hedland_2006/report/summary.tex @ 3364

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port hedland updates

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1This report has described the impact to Onslow from a tsunami
2generated by a Mw 9 earthquake on the Sunda Arc subduction zone
3occurring at Highest Astronomical Tide, Lowest Astronomical Tide
4and Mean Sea Level.
5There is no knowledge of the return period for this event. The
6modelling methodology, assumptions and data sources for the Onslow
7scenario have also been described.
8As discussed in Section \ref{sec:issues}, it is imperative
9that the best available data is used to increase confidence
10in the inundation maps. An onshore grid resolution of the order
11of tens of metres is required, however, it is more important that the data
12is accurate (or at least well known).
13These scenarios will be revisited once the probabilistic models
14are complete so that a suite of tsunami impact assessments can be made.
15
16Future activities to support the impact studies on the North West Shelf
17include:
18
19\begin{itemize}
20\item Sourcing of data sets,
21\item Investigation of solution sensitivity to cell resolution,
22bathymetry and tsunami source uncertainties,
23\item Location of boundary for simulation study area, and
24\item Investigation of friction coefficients.
25\end{itemize}
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