Tsunami Wave Breaking
Tsunami Wave Breaking is a hydrodynamic phenomenon characterized by the disintegration of a tsunami wave into turbulent surges upon nearing shallow coastal regions, distinguished from ordinary wave breaking by its occurrence at continental shelf scales and its dependence on nonlinear amplitude amplification rather than wind-driven wave instability.
318
Publications
17K
Citations
881
Authors
433
Institutions
Publications per year
2017–2026
68
Parents
318
Field Survey of the 27 February 2010 Chile Tsunami
Hermann M. Fritz, Catherine Petroff, Patricio A. Catalán et al. · Pure and Applied Geophysics · 2011 · 338 citations
1–5 of 318
881
Institute of Oceanology. PP Shirshov Russian Academy of Sciences, Russia
21 publications · 1.3K citations
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10
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9
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9
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9
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1–5 of 881
433
Fisheries and Oceans Canada
Ottawa, Canada
18 h-index
46 publications
2.4K citations
Institute of Oceanology. PP Shirshov Russian Academy of Sciences
Moscow, Russia
18 h-index
30 publications
1.4K citations
University of Southern California
Los Angeles, United States
18 h-index
36 publications
3.7K citations

Tohoku University
Sendai, Japan
12 h-index
28 publications
1.5K citations

Centre National de la Recherche Scientifique
Paris, France
10 h-index
31 publications
2.1K citations
Institute of Applied Physics
Nizhny Novgorod, Russia
10 h-index
13 publications
569 citations

University of Bologna
Bologna, Italy
9 h-index
23 publications
2.1K citations
Russian Academy of Sciences
Moscow, Russia
8 h-index
8 publications
168 citations
1–8 of 433
PAGEOPH · 65 publications · 3.2K citations
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30 publications · 1.6K citations
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23 publications · 1.5K citations
18
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17 publications · 1.5K citations
17
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16 publications · 578 citations
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