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Numerical simulation of Langmuir circulations in a wavy domain and its comparison with the Craik-Leibovich theory.

机译:波浪域Langmuir环流的数值模拟及其与Craik-Leibovich理论的比较。

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Numerical simulations of laminar and turbulent open channel flows under a moving wavy surface that has the form of a second order Stokes wave are performed. A constant tangential stress imposed at the top drives a mean current that interacts with the surface wave and generates Langmuir circulations. The Navier-Stokes equations are solved in a curvilinear coordinate system with a modified version of the fractional step method of Zang et al. (1994). Large eddy simulation is used for turbulent flows with the sub-grid stresses modeled with a dynamically determined Smagorinsky constant.; First, two components of the velocity field important to Langmuir circulations are identified in two dimensional free wavy surface flows: the Stokes drift caused by the irrotational wave motion, and the Eulerian mean flow induced by the top wavy boundary layer.; Numerical simulations based the Craik-Leibovich (CL) theory show that the second order Eulerian mean flow induced by the surface is essential in predicting the correct quantitative properties of Langmuir circulations, especially the pitch, defined as the ratio of the maximum downwind jet velocity to the maximum downwelling velocity. In laminar flows, with the Eulerian mean flow effect included, excellent agreement is achieved between the computed streamwise-averaged wavy flow and that predicted by the CL theory. The averaging in the CL theory is thus justified.; For the turbulent case, the Langmuir circulations are embedded in a much stronger, chaotic instantaneous field; nonetheless, they can be identified by time averaging. In Langmuir turbulence, the mixing due to the turbulence and the mean Langmuir circulations are approximately of equal importance. Relative to turbulent Couette flows, the logarithmic region near the bottom wall is modified and most of the logarithmic profile near the surface is destroyed by the Langmuir circulation, leading to a more uniform mean current. Furthermore, the production of turbulence is enhanced in the top surface layer and the pressure transport term is significant. Although the Langmuir circulation structure is similar in turbulent wavy flow and the flow from the CL theory, the CL theory produces stronger Langmuir cells but weaker turbulence.
机译:对层流和湍流明渠在具有第二阶斯托克斯波形式的移动波浪表面下的流动进行了数值模拟。施加在顶部的恒定切向应力会驱动平均电流,该平均电流与表面波相互作用并产生Langmuir环流。 Navier-Stokes方程是在曲线坐标系中使用Zang等人的分数阶跃方法的改进版本求解的。 (1994)。大涡模拟用于湍流,其子网格应力以动态确定的Smagorinsky常数建模。首先,在二维自由波浪表面流中确定了对Langmuir循环重要的速度场的两个分量:由无旋波运动引起的斯托克斯漂移,以及由顶部波浪边界层引起的欧拉平均流。基于Craik-Leibovich(CL)理论的数值模拟表明,由地面引起的二阶欧拉平均流对于预测Langmuir环流的正确定量特性(尤其是俯仰角)至关重要,后者被定义为最大顺风射流速度与最大下降速度。在层流中,考虑到欧拉平均流效应,在计算得到的流平均波浪流与CL理论预测的流之间实现了极好的一致性。因此,CL理论中的平均是合理的。对于湍流情况,朗缪尔环流被嵌入到一个更强的混沌瞬时场中。尽管如此,它们可以通过时间平均来识别。在朗缪尔湍流中,由于湍流和平均朗缪尔环流而产生的混合具有大致相同的重要性。相对于库埃特湍流,底壁附近的对数区域被修改,地表附近的大多数对数轮廓被朗缪尔环流破坏,从而导致平均电流更均匀。此外,在顶表面层中湍流的产生得到增强,并且压力传递项很重要。尽管Langmuir循环结构在湍流波浪流和CL理论的流中相似,但CL理论产生的Langmuir细胞更强,但湍流却更弱。

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