source: production/onslow_2006/report/anuga.tex @ 3241

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1
2The software tool, ANUGA \cite{ON:modsim}, has been used to develop the
3inundation extent
4and associated water level at various points in space and time.
5ANUGA has been developed by GA and the Australian National University
6(ANU) to solve the nonlinear shallow water
7wave equation using the finite volume technique.
8An advantage of this technique is that the cell area can be changed
9according to areas of interest and that wetting and drying
10is treated robustly as part of the numerical scheme.
11ANUGA is continually being developed and validated to ensure
12the modelling approximations reflect new theory or
13available experimental data sets.
14As such, the current results represent ongoing work
15and may change in the future.
16
17The following set of information is required to undertake the
18inundation modelling;
19
20\begin{itemize}
21\item onshore and offshore elevation data (topographic and bathymetric data,
22see Section \ref{sec:data})
23\item initial conditions, such as initial water levels (e.g. determined by tides)
24\item boundary condition (the tsunami source as described in
25Section \ref{sec:tsunamiscenario})
26\item computational requirements relating to the mesh construction
27\end{itemize}
28
29The initial condition used for this scenario is 0m Australian Height Datum
30which is approximately equal to Mean Sea Level.
31The dynamics of
32tidal effects (that is, the changes in water height over time for
33the entire study area) is not currently modelled.
34Bottom friction will generally provide resistance to the water flow
35and thus reduce the impact somewhat. However, it is an open area
36of research on how to determine the friction coefficients, and
37thus it has not been incorporated
38in the scenario presented in this report. Therefore, the
39results presented are over estimated to some degree.
40
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