11th March Japanese tsunami
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| + | ==== Google Earth KML files for the results in the paper above (Figure 15) ==== | ||
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| + | * [http://gfs.sf.net/tmp/tsunami/reached.kml Predicted boundary of areas reached by the wave] | ||
| + | * [http://gfs.sf.net/tmp/tsunami/inundated.kml Predicted inundated areas after 10 hours] | ||
| == Original simulations (March 2011) == | == Original simulations (March 2011) == | ||
Revision as of 22:20, 19 February 2012
A more recent version of these simulations is presented in
S. Popinet - Adaptive modelling of long-distance wave propagation and fine-scale flooding during the Tohoku tsunami
- Natural Hazards and Earth System Sciences , 2012
- Bibtex
Contents |
Google Earth KML files for the results in the paper above (Figure 15)
Original simulations (March 2011)
- Initial simulation using a crude source model based on CMT solution.
- Refined simulation using a detailed seismic inversion.
Inundation maps
These maps were generated directly from the results of the refined simulation. The spatial resolution in flooded areas is automatically adapted down to ~500 m. Note that the topography is defined using the ETOPO-1 data (1 arcminute i.e. ~1.8 km). The results below could be improved using higher-resolution topographic data (e.g. STRM).
In all Gerris results, the colorscale encodes the log of the maximum wave elevation reached over 5 hours.
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