Modulation instability of Stokes wave → freak wave
By A. Dyachenko, Vladimir E Zakharov. 2005
157 citations recorded by the source corpus.
Subfields: Earth-Surface Processes, Oceanography
View Paper: https://www.semanticscholar.org/paper/bf62dea0c90b98eb927b9285ba1863bca13f69d1
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In Earth-Surface Processes
In Oceanography
Citations in the corpus
- Freak waves as nonlinear stage of Stokes wave modulation instability (2006, background): “[47,58] the nonlinear stage of modulation instability for Stokes waves of steepness μ = ka 0.”
- Numerical modeling of extreme rogue waves generated by directional energy focusing (2007, background): “This energy focusing, in addition to a ‘‘natural’’ occurrence through self-focusing (sideband instability [1,36,52,18], see below), may be due or reinforced by multiple factors, such as an opposing current [43], bottom topography in shallow water [33], frequential [8] and/or directional focusing [6,”
- Instabilities, breathers and rogue waves in optics (2014, result): “from noise results in a series of high-contrast peaks of random intensity [17,18], and it is these localised peaks that have been compared with similar structures seen in studies of ocean rogue waves [2,19,20]. Significantly, the MI growth and decay dynamics in the NLSE have exact solutions in the f”