Changeset 3016


Ignore:
Timestamp:
May 30, 2006, 12:08:03 PM (18 years ago)
Author:
sexton
Message:

fixups

Location:
production/onslow_2006/report
Files:
3 edited

Legend:

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  • production/onslow_2006/report/introduction.tex

    r3015 r3016  
    66coastline to tsunamigenic earthquakes originating from
    77the Sunda Arc subduction zone. There is
    8 historic evidence of such events, \bibitem{CB:ausgeo},
     8historic evidence of such events, \cite{CB:ausgeo},
    99and FESA has sought to assess
    1010the relative risk of its urban and regional communities to the tsunami
     
    2424ANUGA has been developed by GA and the Australian National University
    2525(ANU) to solve the nonlinear shallow water
    26 wave equation using the finite volume technique (described in \cite{ON:modsim}).
     26wave equation using the finite volume technique
     27(described in \cite{ON:modsim}).
    2728An advantage of this technique is that the cell resolution can be changed
    2829according to areas of interest and that wetting and drying
  • production/onslow_2006/report/onslow_2006_report.tex

    r3007 r3016  
    121121     
    122122   \section{References}
     123   \input{references}
    123124
    124125   \section{Metadata}
  • production/onslow_2006/report/tsunami_scenario.tex

    r3015 r3016  
    22to develop the preliminary tsunami hazard assessment which
    33was delivered to FESA in September 2005,
    4 \bibitem{CB:FESA}. In that assessment, a suite of
     4\cite{BC:FESA}. In that assessment, a suite of
    55tsunami were evenly spaced along the Sunda Arc subduction zone and there
    66was no consideration of likelihood. Other sources were not considered, such
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