source: production/onslow_2006/report/data.tex @ 3270

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updates to Onslow report

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1The calculated run-up height and resulting inundation ashore is determined by
2the input topographic and bathymetric elevation, the forcing terms, the
3initial and boundary conditions, as well as the cell area of the computational
4mesh.
5Ideally, the data should adequately capture all complex features
6of the underlying bathymetry and topography and that mesh
7is commensurate with the underlying data, as discussed in
8Section \ref{sec:anuga}. Any limitations
9in the resolution and accuracy of the data will introduce
10errors to the inundation maps, in addition to the range of approximations
11made within the model.
12
13Data for this study have been sourced from a number of agencies. With
14respect to the onshore data, the Defence Imagery and Geospatial
15Organisation (DIGO) supplied the DTED (Digital Terrain Elevation
16Data) Level 2 data which has been authorised for Australian Tsunami
17Warning System use only. This data has a resolution of 1 second
18(about 30 metres), produced from 1:50 000 contours, elevations and
19drainage. In addition, the Department of Land Information (DLI) has provided a
2020m Digital Elevation Model (DEM) and orthophotography
21covering the NW Shelf. The DTED Level 2 data is ``bare earth'' with
22the DLI data is distored by vegetation and buildings. The WA DLI data
23is used for the simulation results which follow, due to its overall
24increased accuracy over the DTED data. Further discussion on the comparison
25between these data sets is deferred to Section \ref{sec:issues}.
26%However, the 30m
27%DTED Level 2 data is ``bare earth'' whereas the DLI data is distorted by
28%vegetation
29%and buildings so we have chosen to use the DTED as the onshore
30%topographic data set. It is also important to note that the DEM does
31%not include features such as rock walls, berths etc.
32
33With respect to the offshore data, the Department of Planning and
34Infrastructure (DPI) have provided state digital fairsheet data around
35Onslow. This data covers only a very small geographic area. (Note,
36similar data has been provided for Pt Hedland and Broome by DPI.)
37The Australian Hydrographic Office (AHO) has supplied extensive
38fairsheet data which has also been utilised.
39The coastline has been generated by
40using the aerial photography and two detailed surveys provided
41by WA DPI. The WA DLI data surrounding the coast is error prone and
42has been clipped at the derived coastline. {\bf confirm}
43Appendix \ref{sec:metadata} provides more details and metadata for data
44used for this study.
45Table \ref{table:data} summarises the available data for this study.
46
47\begin{table}
48\caption{Available data for the North West shelf tsunami inundation studies.}
49\label{table:data}
50\begin{center}
51\begin{tabular}{|l|l|}\hline
52Data & Detail \\ \hline 
53DIGO DTED Level 2  & Onshore, 1 second $\approx$ 30m \\ \hline 
54DLI & Onshore, 20m DEM and orthophotography \\ \hline
55DPI & Offshore, fairsheet data around Onslow \\ \hline
56AHO & Offshore, fairsheet data for North West Shelf region \\ \hline
57\end{tabular}
58\end{center}
59\end{table}
60
61%\begin{figure}[hbt]
62%
63%  \centerline{ \includegraphics[width=100mm, height=75mm]
64%{../report_figures/onslow_data_extent.png}}
65%
66%  \caption{Data extent for Onslow scenario. Offshore data shown in blue
67%and onshore data in green.}
68%  \label{fig:onslowdataarea}
69%\end{figure}
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