Changeset 5242 for anuga_work/publications
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- Apr 24, 2008, 7:30:33 PM (17 years ago)
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anuga_work/publications/anuga_2007/anuga_validation.tex
r5235 r5242 3 3 \documentclass[12pt,a4paper]{article} 4 4 5 % create a pdf of this doc by using pdflatex 5 % create a pdf of this doc by using pdflatex 6 6 % Do \emph{not} change the width nor the height of the text from the 7 7 % defaults set by this document class. … … 22 22 \usepackage{amsfonts} 23 23 \usepackage{underscore} 24 \usepackage{epstopdf} 24 25 % Avoid loading unused packages (as done by some \LaTeX\ editors). 25 26 … … 34 35 \textsc{Australia}. \protect\url{mailto:Duncan.Gray@ga.gov.au}}\footnotemark[1] 35 36 \and 36 T.~Baldock\thanks{University of Queensland, Brisbane, \textsc{Australia}. 37 T.~Baldock\thanks{University of Queensland, Brisbane, \textsc{Australia}. 37 38 \protect\url{mailto:tom.baldock@uq.edu.au}}\footnotemark[2] 38 39 \and 39 40 O.~M.~Nielsen\footnotemark[1] 40 \and 41 \and 41 42 M.~J.~Sexton\footnotemark[1] 42 43 \and … … 84 85 The core of \ANUGA{} is a \Python{} implementation of a finite-volume method 85 86 for 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. 87 In this paper we describe the model, the architecture and a range of 88 validations that have been carried out to establish confidence in the model. 88 89 89 90 … … 142 143 described in section~\ref{sec:fvm}. A more complete discussion of the 143 144 method can be found in \cite{modsim2005} where the model and solution 144 technique is validated on a standard tsunami benchmark data set 145 technique is validated on a standard tsunami benchmark data set 145 146 or in \cite{Roberts2007} where parallelisation of ANUGA is discussed. 146 147 This modelling capability is part of … … 148 149 understand the potential impact from natural hazards in order to 149 150 reduce their impact on Australian communities (see \cite{Nielsen2006}). 150 \ANUGA{} is currently being trialled for flood 151 \ANUGA{} is currently being trialled for flood 151 152 modelling (see \cite{Rigby2008}). 152 153 … … 482 483 wave specifications. The dataset also contained water depth time 483 484 series 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. 485 inundation area. The \ANUGA{} model comprised $41404$ triangles 486 and took about $2000$ s to run on a standard PC or $1500$ s 487 on a 64-bit Opteron 2000 series Linux server. 487 488 488 489 Figure~\ref{fig:val} compares the observed wave tank and modelled … … 501 502 This successful replication of the tsunami wave tank simulation on a 502 503 complex 3D beach is a positive first step in validating the \ANUGA{} 503 modelling capability. 504 modelling capability. 504 505 505 506 \subsection{Manning's Friction Model Validation} 506 507 507 508 % Validation UQ friction 508 509 % at X:\anuga_validation\uq_friction_2007 … … 515 516 \end{figure} 516 517 517 The bed friction is modelled in ANUGA using the Manning's 518 The bed friction is modelled in ANUGA using the Manning's 518 519 model. Validation of this model was carried out by comparing results 519 520 from ANUGA against experimental results from flume wave tanks. The 520 521 experiments were carried out at the Gordon McKay Hydraulics Laboratory 521 522 at 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 526 527 527 528 \subsection{Stage and Velocity Validation in a Flume} … … 566 567 Figure~\ref{fig:uq-flume-depth} show that ANUGA predicts the actual 567 568 water depth very well, with the exception of the fluid tip-region. The 568 water velocity is also predicted accurately. 569 water velocity is also predicted accurately. 569 570 570 571 \subsection{Runup of Solitary wave on circular island wavetank validation}
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