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Spatial Evolution of Laboratory Generated Freak Waves in Deep water Depth

机译:实验室产生的深水怪胎波的空间演化

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In the present paper experimental generated Freak Waves are investigated as they are defiend as transient waves existing in one certain location in one definite instant in time (Kaldenhoff & Schlurmann, 1999). Freak Waves occur due to superposition of numerous wave components of a real sea state and are typically characterized by an extreme waveheight. Moreover, it is determined that Freak Waves are sometimes identified by spilling breaking (Schlurmann, 1999 or Kway et al., 1998). The characteristics of Freak Waves were investigated in spatial domain. Interestingly, laboratory generated waves with extreme waveheights show significant similarities to results from field observations from real sea states, e.g. observed by Sand et al. (1989), Yasuda et al. (1997) or Rozario et al. (1993).
机译:在本文中,实验生成的怪物波浪被调查,因为它们是一个在一个明确的即时存在的某个位置存在的瞬态波浪(Kaldenhoff&Schlurmann,1999)。由于真正的大海状态的众多波部件的叠加而发生怪异波浪,并且通常是一个极端波浪的特征。此外,确定有时通过泄漏破碎(Schlurmann,1999或Kway等,1998)来确定怪异波浪。在空间域中研究了怪胎波的特征。有趣的是,具有极端波浪的实验室产生的波浪表现出显着的相似之处,从真实海区的现场观察结果,例如, Sand等人观察。 (1989),Yasuda等。 (1997)或rozario等。 (1993)。

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