Changeset 7253

Timestamp:

Jun 23, 2009, 4:24:01 PM (15 years ago)

Author:

ole

Message:

Addressed David's comments and fixed some other typos as well
Changed some figure sizes slightly for formatting reasons

Location:

anuga_work/publications/boxing_day_validation_2008

Files:

• patong_validation.tex (modified) (11 diffs)
• tsunami07.bib (modified) (2 diffs)

anuga_work/publications/boxing_day_validation_2008/patong_validation.tex

@@ -81 +81 @@
 to solve the governing equations. However any legitimate model must
 address each of the three distinct stages of tsunami evolution---
-generation, propagation and inundation. Geological models must be used
+generation, propagation and inundation. Models combining observed seismic, 
+geodetic and sometimes tsunami data must be used
 to provide estimates of initial sea floor and ocean surface
 deformation. The complexity of these models range from empirical to
@@ -171 +172 @@
 benchmark to validate an operational tsunami inundation model called
 \textsc{anuga} used by Geoscience Australia. A description of
-\textsc{anuga} is given in Secion~\ref{sec:models} and the validation
-results are given in Secion~\ref{sec:results}.
+\textsc{anuga} is given in Section~\ref{sec:models} and the validation
+results are given in Section~\ref{sec:results}.
 
 The numerical models used to model tsunami are extremely
@@ -208 +209 @@
 by the 2004 Sumatra--Andaman earthquake.
 
-The 2004 Sumatra--Andaman tsunami was generated by severe coseismic
+The 2004 Sumatra--Andaman tsunami was generated by a severe coseismic
 displacement of the sea floor as a result of one of the largest
 earthquakes on record. The mega-thrust earthquake started on the 26
@@ -300 +301 @@
 \begin{center}
 \includegraphics[width=0.75\textwidth,keepaspectratio=true]{nested_grids}
-\caption{Nested grids of elevation data.}
+\caption{Nested grids of the elevation data.}
 \label{fig:nested_grids}
 \end{center}
@@ -415 +416 @@
 and third waves approaching and further flooding the buildings and
 street.  The first video is in the very north filmed from what is
-believed to be the roof of the Novotel Hotel marked 'North' in Figure
+believed to be the roof of the Novotel Hotel marked ``north'' in Figure
 \ref{fig:gauge_locations}. The second video is in the very south
 filmed from the second story of a building next door to the Comfort
 Resort near the corner of Ruam Chai St and Thaweewong Road.  This
-location is marked 'south' in Figure \ref{fig:gauge_locations} and
+location is marked ``south'' in Figure \ref{fig:gauge_locations} and
 Figure~\ref{fig:video_flow} shows stills from this video. Both videos
-were used to estimate flow speeds and inundation dephts over time.
-
-\begin{figure}[ht]
-\begin{center}
-\includegraphics[width=6.0cm,keepaspectratio=true]{flow_rate_south_0_00sec.jpg}
-\includegraphics[width=6.0cm,keepaspectratio=true]{flow_rate_south_5_04sec.jpg}
-\includegraphics[width=6.0cm,keepaspectratio=true]{flow_rate_south_7_12sec.jpg}
-\includegraphics[width=6.0cm,keepaspectratio=true]{flow_rate_south_7_60sec.jpg}
+were used to estimate flow speeds and inundation depths over time.
+
+\begin{figure}[ht]
+\begin{center}
+\includegraphics[width=5.0cm,keepaspectratio=true]{flow_rate_south_0_00sec.jpg}
+\includegraphics[width=5.0cm,keepaspectratio=true]{flow_rate_south_5_04sec.jpg}
+\includegraphics[width=5.0cm,keepaspectratio=true]{flow_rate_south_7_12sec.jpg}
+\includegraphics[width=5.0cm,keepaspectratio=true]{flow_rate_south_7_60sec.jpg}
 \caption{Four frames from a video where flow rate could be estimated,
   circle indicates tracked debris, from top left: 0.0 sec, 5.0 s, 7.1
@@ -481 +482 @@
 waveheights and velocities but the authors are not aware of the
 availability of such data.
+
 
 
@@ -602 +604 @@
 then solved using the semi-discrete central-upwind scheme of Kurganov
 et al~\cite{kurganov01} for solving one-dimensional conservation
-equations. The numerical scheme is presented in detail in Zoppou and
-Roberts~\cite{zoppou99}, Roberts and Zoppou~\cite{roberts00}, and
+equations. The numerical scheme is presented in detail in 
+Roberts and Zoppou~\cite{zoppou99,roberts00} and
 Nielsen et al~\cite{nielsen05}. An important capability of the
 software is that it can model the process of wetting and drying as
@@ -721 +723 @@
 the approximated ocean and surface elevation and horisontal flow
 velocities were extracted and used to construct a boundary condition
-for the \textsc{anuga} model. The interface betwen the \textsc{ursga}
+for the \textsc{anuga} model. The interface between the \textsc{ursga}
 and \textsc{anuga} models was chosen to roughly follow the 100 m depth
 contour along the west coast of Phuket Island. The computational
@@ -997 +999 @@
 number of existing benchmarks, the proposed test validates all three
 stages of tsunami evolution - generation, propagation and
-inundation. In an attempt to provide higher visability and easier
+inundation. In an attempt to provide higher visibility and easier
 accessibility for tsunami benchmark problems the data used to
 construct the proposed benchmark is documented and freely available at
@@ -1025 +1027 @@
 of Mathematics, The Australian National University. The authors would
 like to thank Niran Chaimanee from the CCOP, Thailand for providing
-the post 2004 tsunami survey data, building footprints, aereal
+the post 2004 tsunami survey data, building footprints, aerial
 photography and the elevation data for Patong beach, Prapasri Asawakun
 from the Suranaree University of Technology and Parida Kuneepong for
@@ -1034 +1036 @@
 \section{Appendix}
 
-This appendix present the images used to asses the model sensitivities described in 
+This appendix present the images used to assess the model sensitivities described in 
 Section~\ref{sec:sensitivity}.
 

anuga_work/publications/boxing_day_validation_2008/tsunami07.bib

@@ -898 +898 @@
 Tmonth = {December},
 organization = {Modelling and Simulation Society of Australia and New Zealand},
-note = {http://www.mssanz.org.au/modsim05/papers/nielsen.pdf}
+note = {\url{http://www.mssanz.org.au/modsim05/papers/nielsen.pdf}}
 }
 
@@ -1072 +1072 @@
 @Article{wang03,
 author = {Wang, R. and  Martin, F. L.  and Roth, F.},
-title = {Computation of deformation induced by earthquakes in a multi-layered crust – FORTRAN programs EDGRN EDCMP},
+title = "{Computation of deformation induced by earthquakes in a multi-layered crust – FORTRAN programs EDGRN/EDCMP}",
 journal = {Comp. and Geosc.},
 year = {2006},