1 | |
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2 | The modelling has considered three separate regions based on the location |
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3 | of the historical and potential slide failures. The regions A, B and C refer |
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4 | to Wollongong, Sydney and Newcastle. Figure \ref{fig:overallmodel} shows |
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5 | each model with respect to each other and highlights the location |
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6 | of the slides modelled in this study. See Appendix \ref{sec:anugasetup} |
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7 | for the detailed inundation modelling setup for each study region. |
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8 | |
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9 | \begin{figure}[p] |
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10 | \centering |
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11 | \begin{tabular}{cc} |
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12 | \includegraphics[scale=0.4]{../report_figures/overallmodelv3.jpg} & |
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13 | \includegraphics[scale=0.4]{../report_figures/detailedmodel.jpg} \\ |
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14 | (a) & (b) \\ |
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15 | \end{tabular} |
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16 | \caption{(a) NSW region showing the location of study regions A, B and C and the location |
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17 | of the origins of the historical and potential slides. (b) Region C0 developed to allow |
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18 | modelling of the potential slide area withine region C.} |
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19 | \label{fig:overallmodel} |
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20 | \end{figure} |
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21 | |
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22 | The purpose of this section is show the maximum inundation map for each |
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23 | slide scenario for region A, B and C. The Bulli and Shovel slide occurring |
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24 | in region A and the Birubi and Yacaaba slide in region C are considered to have occurred. |
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25 | The potential slides are based on the volumes of these slides located in |
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26 | appropriate locations in the other regions. |
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27 | The outputs in region B and C0 should thus be interpretted as potential tsunami inundation |
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28 | for slides of varied volume. |
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29 | The modelling effectively describes the output as a function of slide |
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30 | volume with Bulli the largest. This event may be used in paleo-tsunami |
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31 | investigations due to occur in early 2007. |
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32 | |
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33 | The time to impact after the initiation of the slide is approximately 25 mins |
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34 | for region A and B and approximately 35 mins for region C. See Appendix \ref{sec:timeseries} |
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35 | for time series outputs at Fairy Meadow (for region A), Manly Beach (for region B) and |
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36 | Stockton Beach (for region C). |
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37 | |
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38 | \begin{table} |
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39 | \begin{center} |
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40 | |
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41 | \caption{Parameters used in ANUGA for the the submarine mass failure scenarios.} |
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42 | \begin{tabular}{|l|l|l|l|l|}\hline |
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43 | {\bf Parameter} & {\bf Bulli} & {\bf Shovel} & {\bf Yacaaba } & {\bf Birubi }\\ \hline |
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44 | Length (m) & 16840 & 13500 & 4189 & 9903 \\ \hline |
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45 | Width (m) & 8860 & 4350 & 2898 & 4150 \\ \hline |
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46 | Thickness (m) & 424 & 165 & 53 & 140 \\ \hline |
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47 | Density g m$^{-3}$ & 1.46 & 1.49 & 1.48 & 1.48 \\ \hline |
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48 | Water depth to centre of mass (m) & 1470 & 877 & 938 & 1320 \\ \hline |
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49 | Bathymetric slope (\degree) & 4 & 4 & 2.3 & 3.7\\ \hline |
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50 | Angular orientation (\degree) & 126 & 118 & 133 & 133 \\ \hline |
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51 | \end{tabular} |
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52 | |
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53 | \end{center} |
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54 | \end{table} |
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55 | |
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56 | Figures \ref{fig:bulliA}, \ref{fig:bulliB}, \ref{fig:bulliC0}, \ref{fig:bulliC} and \ref{fig:bulliC2} |
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57 | describe the inundation extent to regions A, B, C0, C (near historical Birubi) and C |
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58 | (near historical Yacaaba) respectively |
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59 | for the Bulli volume, noting that \ref{fig:bulliA} is the historical event. |
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60 | Similarly, Figures \ref{fig:shovelA}, \ref{fig:shovelB}, \ref{fig:shovelC0}, \ref{fig:shovelC} |
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61 | and \ref{fig:shovelC2} describe the inundation extent for the Shovel |
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62 | volume, noting that \ref{fig:shovelA} is the historical event. |
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63 | Figures \ref{fig:yacaabaA}, \ref{fig:yacaabaB}, \ref{fig:yacaabaC0}, \ref{fig:yacaabaC} and |
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64 | \ref{fig:yacaabaC2} describe the inundation extent for the Yacaaba volume, noting |
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65 | that \ref{fig:yacaabaC2} is the historical event. |
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66 | Figures \ref{fig:birubiA}, \ref{fig:birubiB}, \ref{fig:birubiC0}, \ref{fig:birubiC} and |
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67 | \ref{fig:birubiC2} describe the inundation extent for the Birubi volume, noting |
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68 | that \ref{fig:birubiC} is the historical event. |
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69 | It appears that the inundation extent grows with the volume of the slide. This may |
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70 | be explained through Figure \ref{fig:depthvsamp} where the |
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71 | characteristic three dimensional |
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72 | amplitude is shown as a function of depth for each |
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73 | slide volume (see Appendix \ref{sec:smfmodel} for details). The depth |
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74 | for each specific slide is marked on the curve corresponding to its volume. From this we |
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75 | can see that the initial amplitude is greatest for the Bulli slide, followed by the Shovel and Birubi |
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76 | slides. |
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77 | |
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78 | |
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79 | \begin{figure}[p] |
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80 | %\centerline{\includegraphics[scale=0.25]{../report_figures/depthvsampdataslide.png}} |
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81 | \caption{Relationship between characteristic 3D amplitude and depth |
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82 | for each slide volume.} |
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83 | \label{fig:depthvsamp} |
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84 | \end{figure} |
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