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Research of a neutral and stable boundary layer of the atmosphere using an explicit algebraic model of Reynolds stresses

机译:雷诺应力明确代数模型对大气中立和稳定边界层的研究

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An explicit anisotropic algebraic model of the Reynolds stresses and the turbulent heat flux is tested in a neutrally stratified and stably stratified atmospheric boundary layer (ABL) over a homogeneous rough surface. To construct the algebraic model a three-parameter turbulence model is used, with the help of which the efficiency of eddy mixing of momentum in a neutrally stratified ABL and the efficiency of eddy mixing momentum and heat in a stable stratified atmospheric boundary layer is studied. The being version of the algebraic model is based on the physical principles of the RANS (Reynolds Average Navier Stokes) approximation for describing of stratified turbulence. The model includes the effect of gravitational waves, which allows taking into account the momentum maintenance under strong stability conditions. A comparison of the calculation results with the observational data and other numerical models available in the literature shows that the turbulence model is capable of reproducing the most important structural features for both the neutrally stratified ABL and stably stratified ABL and shows good agreement with the results of LES modeling.
机译:的雷诺应力的显式各向异性代数模型和湍流热通量在一中性分层测试和稳定地在分层的均匀粗糙表面大气边界层(ABL)。为了构建代数模型使用三个参数的湍流模型,与其中的动量涡流混合在一中性分层ABL的效率和涡流混合动量和热量以稳定的效率分层大气边界层被研究的帮助。代数模型的版本是基于RANS(雷诺平均纳维斯托克斯)近似的物理原理的分层湍流的描述。该模型包括引力波,这允许考虑到较强的稳定性的条件下动量维护的效果。该计算结果与可用的观测数据和其他数字模型在文献中示出了湍流模型是能够再现两者的最重要的结构特征的中性分层ABL的且稳定地分层ABL和示出了具有的结果是一致的的比较LES造型。

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