Tsunami Refraction is a hydrodynamic phenomenon in which the propagation direction of a tsunami wave changes due to spatial variations in water depth as the wave approaches coastal regions, distinguishing it from other wave transformation processes by its dependence on the gradient of the seafloor topography.
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2017–2026
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University of Southern California
Los Angeles, United States
3 h-index
4 publications
207 citations
The University of Tokyo
Tokyo, Japan
2 h-index
6 publications
333 citations
Fisheries and Oceans Canada
Ottawa, Canada
2 h-index
3 publications
146 citations
Friedrich Schiller University Jena
Jena, Germany
2 h-index
2 publications
84 citations
James Cook University
Townsville, Australia
2 h-index
3 publications
58 citations
Australian Nuclear Science and Technology Organisation
Sydney, Australia
2 h-index
2 publications
91 citations
Johannes Gutenberg University Mainz
Mainz, Germany
2 h-index
6 publications
150 citations
UNSW Sydney
Sydney, Australia
2 h-index
7 publications
296 citations
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- Pure and Applied Geophysics
PAGEOPH · 7 publications · 416 citations
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- Marine Geology
4 publications · 232 citations
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- Natural Hazards
4 publications · 178 citations
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- Journal of Geophysical Research Atmospheres
JGR · 2 publications · 286 citations
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- Earth-Science Reviews
2 publications · 91 citations
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