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A coupled-mode technique for the transformation of ship-generated waves over variable bathymetry regions

机译:耦合模式技术在可变测深区域上转换舰船产生的波

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In the present work, a coupled-mode technique is applied to the transformation of ship's waves over variable bathymetry regions, characterised by parallel depth-contours, without any mild-slope assumption. This method can be used, in conjunction with ship's near-field wave data in deep water or in constant-depth, as obtained by the application of modern (linearised or non-linear) ship computational fluid dynamic (CFD) codes, or experimental measurements, to support the study of wave wash generated by fast ships and its effects on the nearshore/coastal environment. Under the assumption that the ship's track is straight and parallel to the depth-contours, and relatively far from the bottom irregularity. the problem of propagation-refraction-diffraction of ship-generated waves in a coastal environment is efficiently treated in the frequency domain, by applying the consistent coupled-mode model developed by Athanassoulis and Belibassakis [J. Fluid Mach. 1999;389] to the calculation of the transfer function enabling the pointwise transformation of ship-wave spectra over the variable bathymetry region. Numerical results are presented for simplified ship-wave systems, obtained by the supposition of source-sink Havelock singularities simulating the basic features of the ship's wave pattern. The spatial evolution of the ship-wave system is examined over a smooth but steep shoal, resembling coastal environments, both in the subcritical and in the supercritical case. Since any ship free-wave system, either in deep water or in finite depth, can be adequately modelled by wavecut analysis and suitable distribution of Havelock singularities e.g. as presented by Scrags [21 st Int. Conf. Offshore Mach. Arctic Eng., OMAE2002, Oslo, Norway. June 2002], the present method, in conjunction with ship CFD codes, supports the prediction of ship wash and its impact on coastal areas, including the effects of steep sloping-bed parts.
机译:在目前的工作中,耦合模式技术应用于在可变测深区域的船舶波浪的转换,其特征是具有平行的深度轮廓,无需任何缓坡假设。该方法可以与深水或恒定深度的船舶近场波数据结合使用,如通过应用现代(线性化或非线性)船舶计算流体动力学(CFD)代码或实验测量获得的数据,以支持对快速船舶产生的波浪冲刷及其对近岸/沿海环境的影响的研究。假设船舶的航迹是平直且平行于深度轮廓的,并且距底部不规则处相对较远。通过应用由Athanassoulis和Belibassakis开发的一致耦合模式模型,可以在频域中有效地处理沿海环境中船生波的传播-折射-衍射问题[J.流体马赫。 1999; 389]的传递函数的计算,可以在可变测深区域上进行船舶波谱的逐点变换。提出了简化的船舶波浪系统的数值结果,该假设是通过假设源汇的Havelock奇点模拟船舶的波浪模式的基本特征而获得的。在亚临界和超临界情况下,在一个光滑但陡峭的浅滩上,类似于沿海环境,研究了船浪系统的空间演化。由于任何深海或有限深度的舰船自由波系统都可以通过波形分析和Havelock奇点的适当分布(例如,如Scrags提出的[21st Int。 Conf。离岸马赫。北极工程公司,OMAE2002,挪威奥斯陆。 [2002年6月],本方法结合船舶CFD代码,支持对船舶冲刷及其对沿海地区的影响(包括陡坡床部分的影响)的预测。

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