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anuga_work/publications/boxing_day_validation_2008/patong_validation.tex
r5795 r5884 17 17 $^2$Geoscience Australia, Canberra, Australia\\ 18 18 Email: \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.} 20 20 21 21 \maketitle … … 126 126 127 127 Both 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. 166 129 167 130 168 … … 188 226 \bibitem{roberts00} 189 227 Roberts, 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} 229 Satake, K. (1995). Linear and nonlinear computations of the 1992 Nicaragua earthquake tsunami. Pure and Applied Geophysics, {\bf 144(3)}, 455-470. 190 230 \bibitem{synolakis05} 191 231 Synolakis, 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. … … 204 244 \bibitem{vigny05} 205 245 Vigny, 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} 247 Wang, 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. 206 248 \bibitem{yeh94} 207 249 Yeh, 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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