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On the modeling of equatorial shallow-water waves with the Coriolis effect

机译:论科里奥利效应的赤道浅水波的建模

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In the present study a simplified phenomenological model of shallow-water wave propagating mainly in the equatorial ocean regions with the Coriolis effect caused by the Earth's rotation is formally derived. The model equation which is analogous to the Green-Naghdi equations with the second-order approximation of the Camassa-Holm scaling captures stronger nonlinear effects than the classical dispersive integrable equations like the Korteweg-de Vries and two-component Camassa-Holm system. The local wellposedness of the Cauchy problem is then established by the linear transport theory and wave-breaking phenomenon is investigated based on the method of characteristics and the Riccati-type differential inequality. Finally, the condition of permanent waves is demonstrated by analyzing competition between the slope of average of horizontal velocity component and the free surface component. (C) 2018 Elsevier B.V. All rights reserved.
机译:在本研究中,浅水波主要在赤道海洋区域中传播的简化现象学模型,其具有由地球旋转引起的科里奥利效应进行了衍生。 类似于Camassa-holm缩放的二阶近似的绿色Naghdi方程类似的模型方程捕获比Korteweg-de Vries和双组分Camassa-Holm系统等经典分散的可完整方程更强的非线性效果。 然后通过基于特征方法和Riccati型差速不平等来研究Cauchy问题的局部井接问题。 最后,通过分析水平速度分量和自由表面成分的平均斜率之间的竞争来证明永久波的状况。 (c)2018 Elsevier B.v.保留所有权利。

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