The nonlinear dynamics of rogue waves and holes in deep-water gravity wave trains

By A. Osborne, M. Onorato, M. Serio. 2000

364 citations recorded by the source corpus.

Subfields: Oceanography, Statistical and Nonlinear Physics

View Paper: https://www.semanticscholar.org/paper/d38b693ce4c1eea72e5c4f0ced40af7a592a835e

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In Oceanography

In Statistical and Nonlinear Physics

Citations in the corpus

On the Estimation of the Kurtosis in Directional Sea States for Freak Wave Forecasting (2011, neutral): “Owing to the many research efforts, the occurrence of freak waves, their mechanism, and detailed dynamic properties are now becoming clear (Trulsen and Dysthe 1997; Lavrenov 1998; Osborne et al. 2000; Onorato et al. 2001; Mori et al. 2002).”
On Kurtosis and Occurrence Probability of Freak Waves (2006, background): “As a result of many research efforts, the occurrence of freak waves, their mechanisms, and detailed dynamic properties are now becoming clearer (e.g., Trulsen and Dysthe 1997; Lavrenov 1998; Osborne et al. 2000; Onorato et al. 2001; Haver 2001; Mori et al. 2002).”
Wave breaking onset and strength for two-dimensional deep-water wave groups (2007, background): “Phillips, Gu & Donelan 1993; Osborne, Onorato & Serio 2000 ) are of particular relevance.”
What makes the Peregrine soliton so special as a prototype of freak waves? (2010, background): “Considerable progress has been made, and, on the theoretical front, so far two main generic mechanisms have been identified in the absence of wave-current interaction: the Benjamin–Feir (BF) or modulational instability [1–5] and an essentially linear space-time focussing; see e.”
Extreme waves, modulational instability and second order theory: wave flume experiments on irregular waves (2006, neutral): “analytical solutions (see [41]) of the NLS equations were considered as candidates for rogue waves [25,26,42].”
On Oceanic Rogue Waves (2015, background): “); Fedele (2008); Onorato et al. (2009); Shemer and Sergeeva (2009); Toffoli et al. (2010)), especially in long-crested seas. The wave ﬁeld near a large crest is that of a breather (Peregrine (1983); Osborne et al. (2000), see also Ankiewicz et al. (2009)). One integral statistics used as a measure ”
Physical Mechanisms of the Rogue Wave Phenomenon (2003, background): “Also breather solutions can be periodic in time (Ma-breather) and in space (Akhmediev breather); see for instance, Dysthe & Trulsen (1999) and Osborne et al. (2000).”
On Determining the Onset and Strength of Breaking for Deep Water Waves. Part I: Unforced Irrotational Wave Groups (2002, background): “Of particular relevance to the discussion of wind-forced waves and the statistics and structure of extreme waves in wave groups are the papers of Longuet-Hig-gins (1984), Boccotti et al. (1993), Phillips et al. (1993), and Osborne et al. (2000), among others.”