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Nov 3, 2008, 2:18:58 PM (16 years ago)
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rmleczko
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  • anuga_work/publications/boxing_day_validation_2008/patong_validation.tex

    r5795 r5884  
    1717$^2$Geoscience Australia, Canberra, Australia\\
    1818Email: \href{mailto:jakeman@maths.anu.edu.au}{john.jakeman@anu.edu.au}}
    19 \keywords{ANUGA, Finite Volume Method, Natural Hazards, Indian Ocean Tsunami, Inundation}
     19\keywords{ANUGA, Finite Volume Method, Natural Hazards, Indian Ocean Tsunami, Inundation, Thailand, Phuket, Patong Bay.}
    2020
    2121\maketitle
     
    126126
    127127Both the source models MOST and ... require the input of bathymetric data desribing the geometry of the sea floor. The data used ...
    128 Richard can you add a descrpition here please...
     128       
     129        DBDB2 2 minute of arc grid from the US Naval Research Labs.
     130
     131        This grid was also interpolated to 27 sec of arc and used in a nested grid scheme.
     132
     133
     134        Indian Ocean 27 sec of arc grid created by:
     135
     136        Interpolating the DBDB2 2 minute of arc grid.
     137        In the region where the 9 sec grid sits the data was cut out and replaced by the 9 sec data.
     138        Any points that deviated from the general trend near the boundary were deleted.
     139        The data was then re-gridded.
     140
     141
     142        Andaman Sea 9 sec of arc grid created by:
     143
     144        Sub-sampling the 3 sec of arc grid from NOAA.
     145        In the region where the 3 sec grid sits the data was cut out and replaced by the 3 sec data.
     146        Any points that deviated from the general trend near the boundary were deleted.
     147        The data was then re-gridded.
     148
     149
     150        Thailand off-shore 3 sec of arc grid created by:
     151
     152        cropping a much larger 3 sec of arc grid covering the whole of the Andaman Sea which itself was based on Thai charts 45 and 362.
     153
     154        This grid was obtained from NOAA.
     155
     156        In the region where the 1 sec grid sits the data was cut out and replaced by the 1 sec data.
     157        Any points that deviated from the general trend near the boundary were deleted.
     158        The data was then re-gridded.
     159
     160
     161        Patong Bay 1 second of arc grid created from:
     162
     163        elevation data contained in a GIS of Patong Bay supplied by Niran Chaimanee, Geo-environment Sector Manager, CCOP T/S, Bangkok.
     164
     165        Digitised Thai Navy bathymetry chart no 358.
     166
    129167
    130168
     
    188226\bibitem{roberts00}
    189227Roberts, S.G. and C. Zoppou (2000), Robust and efficent solution of the 2d shallow water wave equation with domains containg dry beds, {\em The ANZIAM Journal}, {\bf 42(E)}, C1260-C1282.
     228\bibitem{satake95}
     229Satake, K. (1995). Linear and nonlinear computations of the 1992 Nicaragua earthquake tsunami. Pure and Applied Geophysics, {\bf 144(3)}, 455-470.
    190230\bibitem{synolakis05}
    191231Synolakis, C., E. Okal, and E. Bernard (2005), The megatsunami of December 26 2004, {\em The Bridge, National Academy of Engineering Publications}, {\bf 35(2)}, 36-35.
     
    204244\bibitem{vigny05}
    205245Vigny, C., W.J.F. Simons, S. Abu, R. Bamphenyu, N. C. Satirapod, C. Subarya Choosakul, A. Socquet, K. Omar, H.Z. Abidin, and B.A.C. Ambrosius (2005), Insight into the 2004 Sumatra-Andaman earthquake from GPS measurements in southeast Asia, {\em Nature}, {\bf 436}, 201-206.
     246\bibitem{wang95}
     247Wang, R., F. L. Martin, et al. (2003). Computation of deformation induced by earthquakes in a multi-layered elastic crust - FORTRAN program EDGRN/EDCMP. Computers and Geosciences, {\bf 29}, 195-207.
    206248\bibitem{yeh94}
    207249Yeh, H., V.V Titov, V. Gusiakov, E. Pelinovsky, V. Khramushin, and V. Kaistrenko (1994), The 1994 Shikotan earthquake tsunami, {\em  Pure and Applied Geophysics}, {\bf 144(3/4)}, 569-593.
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