11th March Japanese tsunami

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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 12(4):1213-1227, 2012
Bibtex

Contents

Google Earth KML files for the results in the paper above (Figure 15)

Original simulations (March 2011)

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.

Comparison between RADARSAT-2 satellite map of standing water bodies (from 12th march 2011) and Gerris results. Sendai area, Miyagi prefecture.
Satellite
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Satellite
Gerris
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Gerris
Comparison between JRC HyFlux2 model results and Gerris results. Wider Sendai area, Miyagi prefecture.
JRC HyFlux2
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JRC HyFlux2
Gerris
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Gerris
Comparison between JRC HyFlux2 model results and Gerris results. Tokai area.
JRC HyFlux2
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JRC HyFlux2
Gerris
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Gerris

See also

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