Changeset 5884

Timestamp:

Nov 3, 2008, 2:18:58 PM (16 years ago)

Author:

rmleczko

Message:

 

Location:

anuga_work/publications/boxing_day_validation_2008

Files:

• 3stages.jpg (added)
• monai-gauge-05-new.png (added)
• most_3_ruptures.png (modified) (previous)
• patong_bay_data.jpg (added)
• patong_validation.pdf (added)
• patong_validation.tex (modified) (4 diffs)

anuga_work/publications/boxing_day_validation_2008/patong_validation.tex

@@ -17 +17 @@
 $^2$Geoscience Australia, Canberra, Australia\\
 Email: \href{mailto:jakeman@maths.anu.edu.au}{john.jakeman@anu.edu.au}}
-\keywords{ANUGA, Finite Volume Method, Natural Hazards, Indian Ocean Tsunami, Inundation}
+\keywords{ANUGA, Finite Volume Method, Natural Hazards, Indian Ocean Tsunami, Inundation, Thailand, Phuket, Patong Bay.}
 
 \maketitle
@@ -126 +126 @@
 
 Both the source models MOST and ... require the input of bathymetric data desribing the geometry of the sea floor. The data used ...
-Richard can you add a descrpition here please...
+        
+        DBDB2 2 minute of arc grid from the US Naval Research Labs.
+
+        This grid was also interpolated to 27 sec of arc and used in a nested grid scheme.
+
+
+        Indian Ocean 27 sec of arc grid created by:
+
+        Interpolating the DBDB2 2 minute of arc grid.
+        In the region where the 9 sec grid sits the data was cut out and replaced by the 9 sec data.
+        Any points that deviated from the general trend near the boundary were deleted.
+        The data was then re-gridded.
+
+
+        Andaman Sea 9 sec of arc grid created by:
+
+        Sub-sampling the 3 sec of arc grid from NOAA.
+        In the region where the 3 sec grid sits the data was cut out and replaced by the 3 sec data.
+        Any points that deviated from the general trend near the boundary were deleted.
+        The data was then re-gridded.
+
+
+        Thailand off-shore 3 sec of arc grid created by:
+
+        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.
+
+        This grid was obtained from NOAA.
+
+        In the region where the 1 sec grid sits the data was cut out and replaced by the 1 sec data.
+        Any points that deviated from the general trend near the boundary were deleted.
+        The data was then re-gridded.
+
+
+        Patong Bay 1 second of arc grid created from:
+
+        elevation data contained in a GIS of Patong Bay supplied by Niran Chaimanee, Geo-environment Sector Manager, CCOP T/S, Bangkok.
+
+        Digitised Thai Navy bathymetry chart no 358.
+
 
 
@@ -188 +226 @@
 \bibitem{roberts00}
 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.
+\bibitem{satake95}
+Satake, K. (1995). Linear and nonlinear computations of the 1992 Nicaragua earthquake tsunami. Pure and Applied Geophysics, {\bf 144(3)}, 455-470.
 \bibitem{synolakis05}
 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}
 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.
+\bibitem{wang95}
+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.
 \bibitem{yeh94}
 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.