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Application of Dynamic Subgrid-scale Models for Large-eddy Simulation of the Daytime Convective Boundary Layer over Heterogeneous Surfaces

机译:动态亚网格尺度模型在非均质表面白天对流边界层大涡模拟中的应用

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摘要

The sensitivity of large-eddy simulation (LES) to the representation of subgrid-scale (SGS) processes is explored for the case of the convective boundary layer (CBL) developing over surfaces with varying degrees of spatial heterogeneity. Three representations of SGS processes are explored: the traditional constant Smagorinsky–Lilly model and two other dynamic models with Lagrangian averaging approaches to calculate the Smagorinsky coefficient (C S ) and SGS Prandtl number (Pr). With initial data based roughly on the observed meteorology, simulations of daytime CBL growth are performed over surfaces with characteristics (i.e. fluxes and roughness) ranging from homogeneous, to striped heterogeneity, to a realistic representation of heterogeneity as derived from a recent field study. In both idealized tests and the realistic case, SGS sensitivities are mostly manifest near the surface and entrainment zone. However, unlike simulations over complex domains or under neutral or stable conditions, these differences for the CBL simulation, where large eddies dominate, are not significant enough to distinguish the performance of the different SGS models, irrespective of surface heterogeneity.
机译:对于在空间异质性程度不同的表面上发展的对流边界层(CBL)的情况,探索了大涡模拟(LES)对子网格规模(SGS)过程表示的敏感性。探索了SGS过程的三种表示形式:传统的常数Smagorinsky-Lilly模型和另外两个具有拉格朗日平均法的动态模型,用于计算Smagorinsky系数(C S )和SGS Prandtl数(Pr)。利用大致基于观测到的气象学的初始数据,可以在具有从均质,条状异质性到真实异质性表示的特征(即通量和粗糙度)到从最近的实地研究中得出的异质性的真实表示的表面上进行白天CBL生长的模拟。在理想化的测试和实际情况下,SGS的敏感性大多表现在表面和夹带附近。但是,与在复杂域上或在中性或稳定条件下进行的仿真不同,对于CBL仿真,在大涡流占主导的情况下,这些差异不足以区分不同SGS模型的性能,而与表面异质性无关。

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