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ANALYSIS OF PROPAGATION OF LONG WAVES IN SHALLOW WATER USING THE KDV-BASED NONLINEAR FOURIER TRANSFORM (KDV-NLFT)

机译:基于KDV的非线性傅里叶变换(KDV-NLFT)分析浅水中长波的传播

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Hydraulic model tests and numerical simulations show that long sinusoidal waves that are generated in very shallow waters are not stable but show modifications of the free surface as function of propagation in time and space. First, with increasing distance from the wave maker the wave becomes asymmetric and develops into a bore-shaped wave. Second, with further increasing distance more and more additional wave crests appear from the front of the bore (undular bore). The shallower the water depth, the more additional wave components can be observed. In extremely shallow water, the periodic sine waves completely disintegrate into periodic trains of solitons. At Leichtweiss-Institute for Hydraulic Engineering and Water Resources (LWI), TU Braunschweig, a nonlinear Fourier transform based on the Korteweg-deVries equation (KdV-NLFT) is implemented and successfully applied in Bruehl that provides an explanation for this nonlinear phenomenon and allows the prediction of the dispersion and propagation of long sinusoidal waves in shallow water.
机译:水力模型测试和数值模拟表明,在非常浅的水中产生的长正弦波不是稳定的,而是显示自由表面随时间和空间的传播而变化。首先,随着与造波器的距离增加,波变得不对称,并发展成孔形波。其次,随着距离的进一步增加,从孔的前方(成孔的孔)会出现越来越多的附加波峰。水深越浅,可以观察到更多的波浪成分。在极浅的水中,周期性的正弦波会完全分解成周期性的孤子列。在不伦瑞克水利工程学院(LWI),不伦瑞克工业大学(TU Braunschweig)实施了基于Korteweg-deVries方程(KdV-NLFT)的非线性傅里叶变换,并将其成功应用于Bruehl中,该变换为这种非线性现象提供了解释并长正弦波在浅水中的扩散和传播的预测。

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