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Experimental demonstration of rogue waves in disordered Luneburg-type photonic networks

机译:无序Luneburg型光子网络中无赖波的实验演示

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A rogue wave, also called freak wave, is a spontaneous phenomenon observed in ocean surface waves. Freak waves are typically defined as waves with a height (trough to crest) that exceed the average wave altitude by a factor of two or more [1]. Although their extreme nature, the first freak wave ever recorder, occurred in 1995 allowing the confirmation of their existence [2]. Similar, extreme, phenomena were soon estimated that could take place in other areas, such as photonics. In this region a freak wave would be an Electromagnetic wave (signal) that would be significantly fiercer than the rest of the signals measured, contiguous to the oceanic phenomenon. Today in the community two main different approaches exist to explain such phenomena, supporting either the linear or the nonlinear wave dynamics interpretations.
机译:流氓波(也称为怪胎波)是在海洋表面波中观察到的自发现象。异常波通常定义为高度(波谷到波峰)超过平均波高两倍或更多的波[1]。尽管它们的极端性质是有史以来的第一个怪胎记录器,但在1995年出现了,从而证实了它们的存在[2]。相似的极端现象很快被估计会发生在其他领域,例如光子学。在该区域中,异常波将是电磁波(信号),该电磁波将比与海洋现象相邻的其余测量信号明显更猛烈。今天,在社区中存在两种主要的不同方法来解释这种现象,它们支持线性或非线性波动动力学的解释。

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