Changeset 4875


Ignore:
Timestamp:
Dec 4, 2007, 5:21:38 PM (16 years ago)
Author:
sexton
Message:

updates to manual - highlighting the hypothetical nature of the Cairns demo

File:
1 edited

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  • anuga_core/documentation/user_manual/anuga_user_manual.tex

    r4874 r4875  
    889889concepts introduced through the \file{runup.py} example and
    890890introduces a second example, \file{runcairns.py}.  This refers to
    891 a real-life scenario, in which the domain of interest surrounds the
     891a {\bf hypothetical} scenario using real-life data,
     892in which the domain of interest surrounds the
    892893Cairns region. Two scenarios are given; firstly, a
    893894hypothetical tsunami wave is generated by a submarine mass failure
    894895situated on the edge of the continental shelf, and secondly, a fixed wave
    895896of given amplitude and period is introduced through the boundary.
     897
     898{\bf
     899Each scenario has been designed to generate a tsunami which will
     900inundate the Cairns region. To achieve this, suitably large
     901parameters were chosen and were not based on any known tsunami sources
     902or realistic amplitudes.
     903}
    896904
    897905\subsection{Overview}
     
    11401148width, thickness, slope, etc), its location (origin) and the depth at that
    11411149location. For this example, we choose to apply the slide function
    1142 at a specified time into the simulation.
     1150at a specified time into the simulation. {\bf Note, the parameters used
     1151in this example have been deliberately chosen to generate a suitably
     1152large amplitude tsunami which would inundate the Cairns region.}
    11431153
    11441154\subsubsection{Friction}
     
    12681278Figures \ref{fig:maxdepthcairnsslide} and \ref{fig:maxdepthcairnsfixedwave} show
    12691279the maximum water depth within the defined region for the slide and fixed wave scenario
    1270 respectively.
     1280respectively. {\bf Note, these inundation maps have been based on purely hypothetical
     1281scenarios and were designed explicitly for demonstration purposes only.}
    12711282The user could develop a maximum absolute momentum or other expressions which can be
    12721283derived from the quantities.
     
    12801291\begin{figure}[hbt]
    12811292\centerline{\includegraphics[scale=0.5]{graphics/slidedepth.jpg}}
    1282 \caption{Maximum inundation map for the Cairns slide scenario.}
     1293\caption{Maximum inundation map for the Cairns slide scenario. \bf Note, this
     1294inundaiton map has been based on a purely hypothetical scenario which was
     1295designed explictiy for demonstration purposes only.}
    12831296\label{fig:maxdepthcairnsslide}
    12841297\end{figure}
     
    12861299\begin{figure}[hbt]
    12871300\centerline{\includegraphics[scale=0.5]{graphics/fixedwavedepth.jpg}}
    1288 \caption{Maximum inundation map for the Cairns fixed wave scenario.}
     1301\caption{Maximum inundation map for the Cairns fixed wave scenario.
     1302\bf Note, this
     1303inundaiton map has been based on a purely hypothetical scenario which was
     1304designed explictiy for demonstration purposes only.}
    12891305\label{fig:maxdepthcairnsfixedwave}
    12901306\end{figure}
     
    13251341Figure \ref{fig:reef} shows the time series for the quantity stage for the
    13261342Elford Reef location for each scenario (the elevation at this location is negative,
    1327 thereby showing stage).
     1343thereby showing stage). Note the large negative stage value when the slide was
     1344introduced. This is due to the double gaussian form of the initial surface
     1345displacement of the slide. By contrast, the time series for depth is shown for the onshore location of the Cairns
     1346Airport for each scenario is Figure \ref{fig:airportboth}.
    13281347
    13291348\begin{figure}[hbt]
     
    13331352\label{fig:reef}
    13341353\end{figure}
    1335 
    1336 By contrast, the time series for depth is shown for the onshore location of the Cairns
    1337 Airport for each scenario is Figure \ref{fig:airportboth}.
    13381354
    13391355\begin{figure}[hbt]
     
    40264042
    40274043This technique can be expanded to handle point data sets as well. In the case
    4028 of a bathymetry data set available in text format in an \code{.xya} file, then
     4044of a bathymetry data set available in text format in an \code{.csv} file, then
    40294045the geospatial addition is updated to
    40304046{\small \begin{verbatim}
    4031 G3 = Geospatial_data(file_name = bathy_data_name + '.xya')
     4047G3 = Geospatial_data(file_name = bathy_data_name + '.csv')
    40324048G = G1 + G2.clip_outside(Geospatial_data(poly1)) + G3
    40334049\end{verbatim}}
    4034 The \code{.xya} file has the data stored as \code{x,y,elevation} with the text \code{elevation}
     4050The \code{.csv} file has the data stored as \code{x,y,elevation} with the text \code{elevation}
    40354051on the first line.
    40364052
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