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Tsunami simulations on several scales: Comparison of approaches with unstructured meshes and nested grids
Harig, S.; Chaeroni; Pranowo, W.S.; Behrens, J. (2008). Tsunami simulations on several scales: Comparison of approaches with unstructured meshes and nested grids. Ocean Dynamics 58(5-6): 429-440.
In: Ocean Dynamics. Springer-Verlag: Berlin; Heidelberg; New York. ISSN 1616-7341, more
Peer reviewed article  

Available in  Authors 

    Bathymetry; Channel capacity; Finite element method; Mathematical models; Satellite altimetry; Shallow water; Shallow water equations; Triangulation; Tsunamis; Marine
Author keywords
    Tsunami; Numerical modeling; Finite element method; Unstructured meshes;Nested grids; Shallow water equations; Model comparison

Authors  Top 
  • Harig, S.
  • Chaeroni
  • Pranowo, W.S.
  • Behrens, J.

    The tsunami event generated by the great Sumatra-Andaman earthquake on 26 December 2004 was simulated with the recently developed model TsunAWI. The model is based on the finite element method, which allows for a very flexible discretization of the model domain. This is demonstrated by a triangulation of the whole Indian Ocean with a resolution of about 14 km in the deep ocean but a considerably higher resolution of about 500 m in the coastal area. A special focus is put on the Banda Aceh region in the Northern tip of Sumatra. This area was heavily hit by the tsunami and the highest resolution in this area is about 40 m in order to include inundation processes in the model simulation. We compare model results to tide gauge data from all around the Indian Ocean, to satellite altimetry, and field measurements of flow depth in selected locations of the Aceh region. Furthermore, we compare the model results of TsunAWI to the results of a nested grid model (TUNAMI-N3) with the same initial conditions and identical bathymetry and topography in the Aceh region. It turns out that TsunAWI gives accurate estimates of arrival times in distant locations and in the same mesh gives good inundation results when compared to field measurements and nested grid results.

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