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Rayleigh wave-internal wave coupling and internal wave generation above a model jet stream

机译:模型射流上方的瑞利波-内波耦合和内波产生

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摘要

Linear theory for modes in a nonuniformly stratified, semi-infinite shear flow demonstrates that Rayleigh waves (stable waves propagating in fluid with spatially varying shear) couple with evanescent internal waves. If the bulk Richardson number (the squared ratio of the buoyancy frequency and shear) lies between 1/4 and 1, the waves have infinite e-folding depth for waves with critical relative horizontal wavenumbers. Fully nonlinear numerical simulations examine the effect of Rayleigh wave-internal wave coupling when the shear layer is localized and is thus Kelvin-Helmholtz unstable. Diagnostics examining profiles of the wave-induced mean now show that if the bulk Richardson number is of order unity, significant momentum is extracted from a shear layer as a consequence of transport by waves. The work is extended to the study of unstable jet flows and applications of this work for internal wave generation by dynamic instability of the upper flank of the jet stream are discussed.
机译:在非均匀分层,半无限剪切流中的模式线性理论表明,瑞利波(稳定波在空间中随着剪切变化而在流体中传播)与e逝的内部波耦合。如果总体理查森数(浮力频率与剪切力的平方比)在1/4与1之间,则对于具有相对相对水平波数的波浪,波浪具有无限大的电子折叠深度。完全非线性的数值模拟研究了当剪切层处于局部且开尔文-亥姆霍兹不稳定时,瑞利波与内部波的耦合作用。诊断检查波诱导平均值的轮廓现在显示,如果总体Richardson数为1阶,则由于波浪传输会从剪切层提取大量动量。这项工作扩展到不稳定射流的研究,并讨论了该工作在射流上部侧面的动态不稳定性内波产生中的应用。

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