Changeset 7470
- Timestamp:
- Sep 2, 2009, 5:28:57 PM (15 years ago)
- Location:
- anuga_work/publications/boxing_day_validation_2008
- Files:
-
- 3 edited
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anuga_work/publications/boxing_day_validation_2008/data.tex
r7468 r7470 8 8 measurements of coseismic displacements as well as bathymetry from ship-based 9 9 expeditions, have now been made 10 available. %~\cite{vigny05,amnon05,kawata05,liu05}. FIXME (Ole): Refs? Are the references here inappropriate?10 available. %~\cite{vigny05,amnon05,kawata05,liu05}. 11 11 12 12 In this section we present the corresponding data necessary to implement … … 173 173 \begin{center} 174 174 \includegraphics[width=8.0cm,keepaspectratio=true]{figures/patong_bay_data.jpg} 175 \caption{3D visualisation of the elevation data set used in Patong Bay showing data points, contours, rivers and roads draped over the final model.} 175 \caption{3D visualisation of the elevation data set used for the nearshore propagation and and inundation in Patong Bay showing 176 digitised data points and contours as well as rivers and roads 177 draped over the data model.} 176 178 \label{fig:patong_bathymetry} 177 179 \end{center} 178 180 \end{figure} 179 FIXME (Jane): legend? Were the contours derived from the final dataset? 180 This is not the entire model, only the bay and the beach. RICHARD 181 181 182 182 183 \subsubsection{Buildings and Other Structures} … … 226 227 \begin{figure}[ht] 227 228 \begin{center} 228 %\includegraphics[width=8.0cm,keepaspectratio=true]{gauge_locations.jpg}229 229 \includegraphics[width=\textwidth,keepaspectratio=true]{figures/gauges.jpg} 230 \caption{Location of timeseries extracted from the model output. FIXME(John): 231 should we combine the inundation map with the gauages map?} 230 \caption{Location of timeseries extracted from the model output.} 231 % FIXME(John): 232 %should we combine the inundation map with the gauages map?} 233 %OLE: No - Kristy and I tried to make each image very simple - 234 %with one message only 232 235 \label{fig:gauge_locations} 233 236 \end{center} -
anuga_work/publications/boxing_day_validation_2008/method.tex
r7450 r7470 137 137 simulating water flow onto a beach or dry land and around structures 138 138 such as buildings. \textsc{Anuga} has been validated against 139 %a number of analytical solutions and 140 %FIXME (Ole): Analytical solutions have not been published. Ask Steve. 139 %a number of analytical solutions !!!Analytical solutions have not been published. Ask Steve. 141 140 the wave tank simulation of the 1993 Okushiri 142 Island tsunami~\cite{nielsen05,roberts06} .143 FIXME (Ole): Add reference to Tom Baldock's Dam Break valiadation of ANUGA.141 Island tsunami~\cite{nielsen05,roberts06} and 142 dam break experiments~\cite{baldock07}. -
anuga_work/publications/boxing_day_validation_2008/results.tex
r7467 r7470 30 30 points) is only 0.06 m, well below the typical error of the 31 31 observations of between 0.25 and 1.0 m. 32 % 33 %However, the occasional point 34 %has quite a large error (over 1 m); for example a couple of 35 %uplifted/subsided points appear to be on a wrong 36 %(FIXME (Jane): This is incorrect) side of the predicted 37 %pivot line~\ref{fig:surface_deformation}. 38 % 32 39 33 The excellence of the fit is 40 34 not surprising, since the original slip model was chosen … … 44 38 uncalibrated source models or source models calibrated on other data 45 39 this test of generation would be more meaningful. 46 %47 %This does demonstrate, however, that \textsc{edgrn} and our modified version of48 %\textsc{edstat} (FIXME(Jane): This has never been mentioned before)49 %can reproduce the correct pattern of vertical50 %deformation very well when the slip distribution is well constrained51 %and when reasonable values for the elastic properties are used.52 53 40 54 41 \begin{figure}[ht] 55 42 \begin{center} 56 43 \includegraphics[width=0.8\textwidth,keepaspectratio=true]{figures/surface_deformation.jpg} 57 %\includegraphics[totalheight=0.3\textheight,width=0.8\textwidth]{surface_deformation.jpg}58 44 \caption{Location and magnitude of the vertical component of the sea 59 45 floor displacement associated with the 2004 Indian Ocean tsunami
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