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Timestamp:
Apr 24, 2008, 7:30:33 PM (17 years ago)
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steve
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  • anuga_work/publications/anuga_2007/anuga_validation.tex

    r5235 r5242  
    33\documentclass[12pt,a4paper]{article}
    44
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    77% defaults set by this document class.
     
    2222\usepackage{amsfonts}
    2323\usepackage{underscore}
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    2526
     
    3435\textsc{Australia}. \protect\url{mailto:Duncan.Gray@ga.gov.au}}\footnotemark[1]
    3536\and
    36 T.~Baldock\thanks{University of Queensland, Brisbane, \textsc{Australia}. 
     37T.~Baldock\thanks{University of Queensland, Brisbane, \textsc{Australia}.
    3738\protect\url{mailto:tom.baldock@uq.edu.au}}\footnotemark[2]
    3839\and
    3940O.~M.~Nielsen\footnotemark[1]
    40 \and 
     41\and
    4142M.~J.~Sexton\footnotemark[1]
    4243\and
     
    8485The core of \ANUGA{} is a \Python{} implementation of a finite-volume method
    8586for solving the conservative form of the Shallow Water Wave equation.
    86 In this paper we describe the model, the architecture and a range of 
    87 validations that have been carried out to establish confidence in the model. 
     87In this paper we describe the model, the architecture and a range of
     88validations that have been carried out to establish confidence in the model.
    8889
    8990
     
    142143described in section~\ref{sec:fvm}.  A more complete discussion of the
    143144method can be found in \cite{modsim2005} where the model and solution
    144 technique is validated on a standard tsunami benchmark data set 
     145technique is validated on a standard tsunami benchmark data set
    145146or in \cite{Roberts2007} where parallelisation of ANUGA is discussed.
    146147This modelling capability is part of
     
    148149understand the potential impact from natural hazards in order to
    149150reduce their impact on Australian communities (see \cite{Nielsen2006}).
    150 \ANUGA{} is currently being trialled for flood 
     151\ANUGA{} is currently being trialled for flood
    151152modelling (see \cite{Rigby2008}).
    152153
     
    482483wave specifications. The dataset also contained water depth time
    483484series from three wave gauges situated offshore from the simulated
    484 inundation area. The \ANUGA{} model comprised $41404$ triangles 
    485 and took about $2000$ s to run on a standard PC or $1500$ s 
    486 on a 64-bit Opteron 2000 series Linux server. 
     485inundation area. The \ANUGA{} model comprised $41404$ triangles
     486and took about $2000$ s to run on a standard PC or $1500$ s
     487on a 64-bit Opteron 2000 series Linux server.
    487488
    488489Figure~\ref{fig:val} compares the observed wave tank and modelled
     
    501502This successful replication of the tsunami wave tank simulation on a
    502503complex 3D beach is a positive first step in validating the \ANUGA{}
    503 modelling capability. 
     504modelling capability.
    504505
    505506\subsection{Manning's Friction Model Validation}
    506  
     507
    507508% Validation UQ friction
    508509% at X:\anuga_validation\uq_friction_2007
     
    515516\end{figure}
    516517
    517  The bed friction is modelled in ANUGA using the Manning's 
     518 The bed friction is modelled in ANUGA using the Manning's
    518519 model. Validation of this model was carried out by comparing results
    519520 from ANUGA against experimental results from flume wave tanks. The
    520521experiments were carried out at the Gordon McKay Hydraulics Laboratory
    521522at St Lucia, University of Queensland.
    522  
    523 %The Manning's friction model is 
    524 
    525 %To validate the friction model 
     523
     524%The Manning's friction model is
     525
     526%To validate the friction model
    526527
    527528\subsection{Stage and Velocity Validation in a Flume}
     
    566567Figure~\ref{fig:uq-flume-depth} show that ANUGA predicts the actual
    567568water depth very well, with the exception of the fluid tip-region. The
    568 water velocity is also predicted accurately. 
     569water velocity is also predicted accurately.
    569570
    570571\subsection{Runup of Solitary wave on circular island wavetank validation}
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