Generation of Vertical Fine Structure by the Internal Waves with the Regard for Turbulent Viscosity and Diffusion

IF 0.7 Q4 OCEANOGRAPHY
A. Slepyshev, A. Nosova
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引用次数: 1

Abstract

Purpose. The aim is to study the mechanism of formation of a vertical fine structure due to the mass vertical transfer by the internal waves taking into account turbulent viscosity and diffusion as well as to investigate influence of the critical layers on the dispersion curves of internal waves. Methods and Results. In the Boussinesq approximation, the free inertia-gravity internal waves in a vertically inhomogeneous flow are considered with the regard for the horizontal turbulent viscosity and diffusion. The equation for the amplitude of vertical velocity of the internal waves contains a small parameter (in the dimensionless variables) proportional to the value of the horizontal turbulent viscosity. The solution of this equation is realized in a form of the asymptotic series of this parameter. In the zero approximation, the second-order homogeneous boundary value problem determined the vertical structure mode is solved numerically by the implicit third-order accuracy Adams scheme for real profiles of the Brent-Väisälä frequency and the current velocity. At the fixed wave frequency, the wave number is determined by the shooting method. In the first order with respect to the indicated parameter, the semi-homogeneous boundary value problem is also solved numerically according to the implicit Adams scheme of the third order of accuracy. A unique solution is found which is orthogonal to the solution of the corresponding homogeneous boundary value problem. The condition of this boundary value problem solvability yields the wave attenuation decrement. The dispersion curves of the first two modes are cut off in the lowfrequency region (the second mode is at a higher frequency), that is due to influence of the critical layers, where the wave frequency with the Doppler shift is inertial. It is shown that the mass vertical wave flux differs from zero and leads to correction (not oscillating on the wave time scale) of the average density, i. e. the internal wave generate fine structure that is of an irreversible character. Conclusions. When the horizontal turbulent viscosity and diffusion are taken into consideration, the mass vertical wave flux differs from zero and leads to generation of the vertical fine structure. The mass wave flux exceeds the turbulent one. The vertical scales of the generated vertical fine structure correspond to the actually observed ones.
考虑湍流黏度和扩散的内波产生垂直精细结构
目的。目的是研究考虑湍流黏度和扩散的内波质量垂直传递导致的垂直精细结构的形成机理,以及临界层对内波色散曲线的影响。方法与结果。在Boussinesq近似中,考虑了自由惯性-重力内波在垂直非均匀流动中的水平黏度和扩散。内波垂直速度振幅的方程包含一个小参数(在无量纲变量中),该参数与水平湍流粘度的值成正比。该方程的解以该参数的渐近级数形式实现。在零逼近条件下,采用隐式三阶精度Adams格式对确定垂直结构模式的二阶齐次边值问题进行了数值求解,得到了Brent-Väisälä频率和当前速度的实际剖面。在固定的波频下,用射波法确定波数。根据隐式三阶精度的Adams格式,对所指示参数的一阶半齐次边值问题进行了数值求解。得到了一个与齐次边值问题的解正交的唯一解。该边值问题可解的条件产生波衰减减量。前两种模式的色散曲线在低频区域被截断(第二种模式在更高频率),这是由于临界层的影响,其中多普勒频移的波频率是惯性的。结果表明,质量纵波通量不等于零,导致平均密度的修正(在波时尺度上不振荡),即内波产生不可逆的精细结构。结论。考虑水平湍流黏度和扩散时,质量垂向波通量不为零,导致垂向细结构的产生。质量波通量大于湍流波通量。生成的垂直精细结构的垂直尺度与实际观测到的垂直尺度相对应。
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来源期刊
Physical Oceanography
Physical Oceanography OCEANOGRAPHY-
CiteScore
1.80
自引率
25.00%
发文量
8
审稿时长
24 weeks
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