source: anuga_work/production/sydney_2006/report/interpretation.tex @ 6842

Last change on this file since 6842 was 4346, checked in by sexton, 18 years ago

slide modelling updates and slide report updates

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