Impulsive Tsunami and Large Runup Along the Sanriku Coast of Japan Produced by an Inelastic Wedge Deformation Model
Author:
Affiliation:
1. Department of Geological Sciences San Diego State University San Diego CA USA
2. Scripps Institution of Oceanography University of California San Diego CA USA
3. National Research Institute for Earth Science and Disaster Resilience Tsukuba Japan
Funder
National Science Foundation
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JB022098
Reference47 articles.
1. A dislocation model of the 1933 Sanriku earthquake consistent with the tsunami waves.
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5. On the form of the momentum equation for shallow water models based on the generalized wave continuity equation
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