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A three-dimensional model for two coupled turbulent fluids: numerical analysis of a finite element approximation

机译:两个耦合湍流流体的三维模型:有限元近似的数值分析

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This article deals with the numerical analysis of a coupled two-fluid Reynolds-averaged Navier-Stokes (RANS) turbulence model, such as atmosphere-ocean flow. Each fluid is modeled by the coupled steady Stokes equations with the equation for the turbulent kinetic energy (TKE). In this model, the eddy viscosities for velocity and TKE depend on the TKE, the production (source) term for the TKEs is only in L-1 and the boundary condition for the TKEs on the interface between the two flows depends quadratically on the difference of velocities. To overcome the lack of regularity, we approximate the initial system by a regularized system, in which the eddy viscosities and source terms for the TKEs are regularized by convolution. We perform a full finite element discretization of the regularized model, combined with a decoupled iterative linearization procedure. We prove that the discrete scheme converges to the continuous scheme for large enough eddy viscosities in natural norms. Finally, we present some numerical tests where we study the accuracy of the procedure, and simulate a realistic flow in which an imposed wind in the upper atmosphere generates an upwelling in the oceanic flow.
机译:本文涉及耦合的双流体雷诺平均纳米斯(RAN)湍流模型的数值分析,例如大气海流。每个流体由耦合的稳态斯托克斯方程式建模,其具有湍流动能(TKE)的等式。在该模型中,用于速度和TKE的涡粘度取决于TKE,TKE的生产(源)术语仅在L-1中,两个流程之间的接口上的TKE的边界条件依赖于差异速度。为了克服规律性缺乏,我们通过正则化系统估计初始系统,其中通过卷积规则化TKE的涡粘度和源术语。我们执行正则化模型的完整有限元离散化,与解耦的迭代线性化过程相结合。我们证明了离散方案会聚到持续方案,以实现自然规范的大足够大的涡粘度。最后,我们介绍了一些数值测试,我们研究了程序的准确性,并模拟了上层大气中的施加风在海洋流动中产生的现实流程。

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