Ruban V P
Landau Institute for Theoretical Physics, 2 Kosygin Street, 119334 Moscow, Russia.
Phys Rev Lett. 2007 Jul 27;99(4):044502. doi: 10.1103/PhysRevLett.99.044502. Epub 2007 Jul 25.
A specific, genuinely three-dimensional mechanism of rogue wave formation, in a late stage of the modulational instability of a perturbed Stokes deep-water wave, is recognized through numerical experiments. The simulations are based on fully nonlinear equations describing weakly three-dimensional potential flows of an ideal fluid with a free surface in terms of conformal variables. Spontaneous formation of zigzag patterns for wave amplitude is observed in a nonlinear stage of the instability. If initial wave steepness is sufficiently high (ka>0.06), these coherent structures produce rogue waves. The most tall waves appear in turns of the zigzags. For ka<0.06, the structures decay typically without formation of steep waves.
通过数值实验,在受扰斯托克斯深水波调制不稳定性的后期阶段,识别出一种特定的、真正三维的异常波形成机制。模拟基于完全非线性方程,该方程用共形变量描述了具有自由表面的理想流体的弱三维势流。在不稳定性的非线性阶段观察到波幅的锯齿形图案的自发形成。如果初始波陡足够高(ka>0.06),这些相干结构会产生异常波。最高的波出现在锯齿的转弯处。对于ka<0.06,这些结构通常会衰减,不会形成陡波。