Changeset 3217


Ignore:
Timestamp:
Jun 23, 2006, 3:41:21 PM (19 years ago)
Author:
sexton
Message:

fixes

Location:
production/onslow_2006
Files:
4 edited

Legend:

Unmodified
Added
Removed
  • production/onslow_2006/make_report.py

    r3215 r3217  
    7676production_dirs = {'20060515_001733': '0 AHD'}
    7777
    78 max_maps = {'1.5 AHD': 'HAT_map',
    79             '-1.5 AHD': 'LAT_map',
    80             '0 AHD': 'MSL_map'}
     78#max_maps = {'1.5 AHD': 'HAT_map',
     79#            '-1.5 AHD': 'LAT_map',
     80#            '0 AHD': 'MSL_map'}
     81
     82max_maps = {'0 AHD': 'MSL_map'}
    8183
    8284#damage_maps = {'1.5 AHD': 'HAT_damage',
     
    165167
    166168\\begin{figure}[hbt]
    167   \centerline{ \includegraphics[scale=0.25]{../report_figures/GAlogo.jpg}}
     169  \centerline{ \includegraphics[scale=0.3]{../report_figures/GAlogo.jpg}}
    168170\end{figure}
    169171   
  • production/onslow_2006/report/anuga.tex

    r3215 r3217  
    4444inundated before the simulation is even begun indicating
    4545shortcomings with the underlying data set. Therefore, we use only
    46 one initial condition for this scenario; 0m AHD.
     46one initial condition for this scenario; 0m AHD. Further
     47discussion surrounding the data and its sources is described in
     48Sections \ref{sec:data} and \ref{sec:metadata}.
    4749%It is important to note that there is no Bureau of Metereoolgy
    4850%tide gauge in Onslow,
  • production/onslow_2006/report/damage.tex

    r3211 r3217  
    2626in Figure
    2727\ref{fig:points}. The population of the Bindibindi community is 140
    28 and is situated below the 1.5m AHD contour as seen in Figure \ref{fig:points}
    29 which indicates it is inundated prior to the tsunami wave arriving.
    30 At 0m AHD, over 3m of water will inundate parts of the community (Figure
     28and is situated close to the coast as seen in Figure \ref{fig:points}.
     29At 0m AHD, over 2m of water will inundate parts of the community (Figure
    3130\ref{fig:gaugeBindiBindiCommunity}) indicating 100\% damage of contents.
    3231
     
    3433residential collapse probability models and casualty models and their
    3534application to inundation modelling.
    36 
    3735
    3836There is a paucity of data on the tsunami vulnerability of buildings.
  • production/onslow_2006/report/interpretation.tex

    r3215 r3217  
    4343(3.8 hours) after the tsunami is generated.
    4444Prior to the drawdown, maximum amplitudes are approximately 50cm at
    45 West of Groyne (Figure \ref{fig:gaugeWestofGroyne}) and the mouth of Beadon Creek
    46 (Figure \ref{fig:gaugeBeadonCreekmouth}), for example. The first wave
     45West of Groyne (Figure \ref{fig:20060515001733gaugeWestofGroyne}) and
     46the mouth of Beadon Creek
     47(Figure \ref{fig:20060515001733gaugeBeadonCreekmouth}), for example.
     48The first wave
    4749after the drawdown ranges from approximatly 2m in the
    48 west of Beadon Bay (Figure \ref{fig:gaugeBeadonBaywest})
    49 to 1.5m in the east of Beadon Bay (Figure \ref{fig:gaugeBeadonBayeast}).
     50west of Beadon Bay (Figure \ref{fig:20060515001733gaugeBeadonBaywest})
     51to 1.5m in the east of Beadon Bay
     52(Figure \ref{fig:20060515001733gaugeBeadonBayeast}).
    5053The speed
    5154sharply increases at drawdown with further increases as the
     
    5962
    6063The maximum speed found for the offshore locations occur at the West of
    61 Groyne location (Figure \ref{fig:gaugeWestofGroyne})
     64Groyne location (Figure \ref{fig:20060515001733gaugeWestofGroyne})
    6265with speeds halved at the Beadon Bay west location.
    6366The Beadon Bay west speed is greater than the east of Beadon
    64 Bay location (Figure \ref{fig:gaugeBeadonBayeast}).
     67Bay location (Figure \ref{fig:20060515001733gaugeBeadonBayeast}).
    6568There is similar differences in amplitude (from drawdown to maximum
    6669amplitude), however, the western location is in deeper water than the eastern
     
    8891transmitted energy of the tsunami wave.
    8992The tsunami wave penetrates the river east of Onslow with wave height
    90 approximately 2m at the mouth (Figure \ref{fig:gaugeBeadonCreekmouth})
     93approximately 2m at the mouth
     94(Figure \ref{fig:20060515001733gaugeBeadonCreekmouth})
    9195and inundation
    9296exceeding 1m found at the Beadon Creek south of dock location (Figure
    93 \ref{fig:gaugeBeadonCreeksouthofdock}).
     97\ref{fig:20060515001733gaugeBeadonCreeksouthofdock}).
    9498%The wave penetrates the river east of Onslow with increasingly
    9599%greater inundation between the -1.5m AHD and 1.5m AHD simulations.
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