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