Changeset 6084
- Timestamp:
- Dec 16, 2008, 3:09:26 PM (15 years ago)
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anuga_work/publications/boxing_day_validation_2008/patong_validation.tex
r6082 r6084 11 11 12 12 %-------authors----------- 13 \author{J.D.~Jakeman$^1$~~and~~O.~Nielsen$^2$~~and~~ K.~VanPutten$^2$~~and~~R.~Mleczko$^2$~~and~~S.G~Roberts$^1$}13 \author{J.D.~Jakeman$^1$~~and~~O.~Nielsen$^2$~~and~~R.~Mleczko$^2$~~and~~K.~VanPutten$^2$~~and~~S.G~Roberts$^1$} 14 14 15 15 %------Affiliation---------- … … 135 135 136 136 Both the source models MOST and ... require the input of bathymetric data desribing the geometry of the sea floor. The data used ... 137 138 The URS code employed 5 nested grids and their creation and data source are described below:139 140 DBDB2 2 minute of arc grid from the US Naval Research Labs.141 142 This grid was also interpolated to 27 sec of arc and used in a nested grid scheme.143 144 145 Indian Ocean 27 sec of arc grid created by:146 147 Interpolating the DBDB2 2 minute of arc grid.148 In the region where the 9 sec grid sits the data was cut out and replaced by the 9 sec data.149 Any points that deviated from the general trend near the boundary were deleted.150 The data was then re-gridded.151 152 153 Andaman Sea 9 sec of arc grid created by:154 155 Sub-sampling the 3 sec of arc grid from NOAA.156 In the region where the 3 sec grid sits the data was cut out and replaced by the 3 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 Thailand off-shore 3 sec of arc grid created by:162 163 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 362.164 165 This grid was obtained from NOAA.166 167 In the region where the 1 sec grid sits the data was cut out and replaced by the 1 sec data.168 Any points that deviated from the general trend near the boundary were deleted.169 The data was then re-gridded.170 171 172 Patong Bay 1 second of arc grid created from:173 174 elevation data contained in a GIS of Patong Bay supplied by Niran Chaimanee, Geo-environment Sector Manager, CCOP T/S, Bangkok.175 176 Digitised Thai Navy bathymetry chart no 358.177 137 178 138 … … 276 236 %===============Appendicis 277 237 278 %\section*{Appendix A. Figures and Tables} 238 \section*{Appendix A. Figures and Tables} 239 240 \subsection (datasets and gridding) 241 242 Gridded data sets used: 243 244 DBDB2 2 minute of arc grid from the US Naval Research Labs. 245 This grid was also interpolated to 27 sec of arc and used in a nested grid scheme. 246 247 Indian Ocean 27 sec of arc grid created by: 248 Interpolating the DBDB2 2 minute of arc grid. 249 In the region where the 9 sec grid sits the data was cut out and replaced by the 9 sec data. 250 Any points that deviated from the general trend near the boundary were deleted. 251 The data was then re-gridded. 252 253 Andaman Sea 9 sec of arc grid created by: 254 Sub-sampling the 3 sec of arc grid from NOAA. 255 In the region where the 3 sec grid sits the data was cut out and replaced by the 3 sec data. 256 Any points that deviated from the general trend near the boundary were deleted. 257 The data was then re-gridded. 258 259 Thailand off-shore 3 sec of arc grid created by: 260 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. 261 This grid was obtained from NOAA. 262 In the region where the 1 sec grid sits the data was cut out and replaced by the 1 sec data. 263 Any points that deviated from the general trend near the boundary were deleted. 264 The data was then re-gridded. 265 266 Patong Bay 1 second of arc grid created from: 267 elevation data contained in a GIS of Patong Bay supplied by Niran Chaimanee, Geo-environment Sector Manager, CCOP T/S, Bangkok. 268 Digitised Thai Navy bathymetry chart no 358. 269 270 The sub-sampling of larger grids was performed by using \bold resample \endbold a GMT program. 271 The gridding of data was performed using \bold Intrepid \endbold a commercial geophysical processing package developed by Intrepid Geophysics. 272 The gridding scheme was nearest neighbour followed by minimum curvature akima spline smoothing. 273 274 \subsection (earthquake source model) 275 276 The earthquake source model of Chlieh was adopted to generate the tsunami simulation. This model was created by carefull inversion of the seismic 277 data and fits both coseismic, tsunami and GPS data in the Andaman Sea well. 278 279 \subsection (tsunami propagation) 280 281 To to generate and propagate the tsunami the URS code was used. This program solves the shallow water equations using the finite difference method. 282 It can also be used in a nexted grid scheme and does on-shore inundation. 279 283 280 284 %%%%%%%%%%%%%%%%%%%%%%%
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