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Study of Near-Surface Models for Large-Eddy Simulations of a Neutrally Stratified Atmospheric Boundary Layer

机译:中层大气边界层大涡模拟的近地表模型研究

摘要

In large-eddy simulations (LES) of the atmospheric boundary layer (ABL), near-surface models are often used to supplement subgrid-scale (SGS) turbulent stresses when a major fraction of the energetic scales within the surface layer cannot be resolved with the temporal and spatial resolution at hand. In this study, we investigate the performance of both dynamic and non-dynamic eddy viscosity models coupled with near-surface models in simulations of a neutrally stratified ABL. Two near-surface models that are commonly used in LES of the atmospheric boundary layer are considered. Additionally, a hybrid Reynolds- averaged/LES eddy viscosity model is presented, which uses Prandtl’s mixing length model in the vicinity of the surface, and blends in with the dynamic Smagorinsky model away from the surface. Present simulations show that significant portions of the modelled turbulent stresses are generated by the near-surface models, and they play a dominant role in capturing the expected logarithmic wind profile. Visualizations of the instantaneous vorticity field reveal that flow structures in the vicinity of the surface depend on the choice of the near-surface model. Among the three near-surface models studied, the hybrid eddy viscosity model gives the closest agreement with the logarithmic wind profile in the surface layer. It is also observed that high levels of resolved turbulence stresses can be maintained with the so-called canopy stress model while producing good agreement with the logarithmic wind profile.
机译:在大气边界层(ABL)的大涡模拟(LES)中,当不能用以下方法解决表面层中大部分能量尺度时,通常使用近地表模型来补充亚网格尺度(SGS)湍流应力。眼前的时空分辨率。在这项研究中,我们研究了中性分层ABL的动态和非动态涡流粘度模型以及近表面模型的性能。考虑了大气边界层LES中常用的两个近地表模型。此外,提出了一个混合的雷诺平均/ LES涡流模型,该模型在表面附近使用Prandtl的混合长度模型,并与远离表面的动态Smagorinsky模型进行融合。当前的模拟表明,建模的湍流应力的很大一部分是由近地表模型生成的,它们在捕获预期的对数风廓线中起着主导作用。瞬时涡度场的可视化结果表明,地表附近的流动结构取决于近地表模型的选择。在研究的三个近地表模型中,混合涡流粘度模型与表层的对数风廓线最接近。还观察到,利用所谓的冠层应力模型可以维持高水平的湍流应力,同时与对数风廓线产生良好的一致性。

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