11th March Japanese tsunami
From Gerris
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| Revision as of 18:12, 1 April 2011 Popinet (Talk | contribs) (Added inundation maps) ← Previous diff |
Revision as of 18:15, 1 April 2011 Popinet (Talk | contribs) (→See also - Added link to parabola test case) Next diff → |
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| * [http://kingkong.amath.washington.edu/clawpack/links/honshu2011/ Geoclaw results] | * [http://kingkong.amath.washington.edu/clawpack/links/honshu2011/ Geoclaw results] | ||
| * [http://gerris.dalembert.upmc.fr/gerris/examples/examples/#htoc18 Validation of Gerris for tsunamis] | * [http://gerris.dalembert.upmc.fr/gerris/examples/examples/#htoc18 Validation of Gerris for tsunamis] | ||
| + | * [http://gerris.dalembert.upmc.fr/gerris/tests/tests/parabola.html More validation of Gerris] | ||
Revision as of 18:15, 1 April 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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