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Large-Eddy Simulation Study of Thermally Stratified Canopy Flow

机译:热分层冠层流的大涡模拟研究

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A number of large-eddy simulations (LES) are performed for the calculation of the airflow over a horizontally homogeneous forest canopy for a wide range of thermal stability classes. For the first time, results from LES of a stably stratified canopy are also presented. Simulation results compare favourably to recent field measurements over a pine forest in south-eastern Sweden. The simple heat source model was found to perform adequately and to yield within-canopy heat-flux profiles typically observed for stable conditions in the field. Evidence was found for a layer of unstably stratified air in the canopy trunk space under stable stratification. The importance of a secondary wind-speed maximum is emphasized in stable conditions. Examination of the budget equation of turbulent kinetic energy (TKE) revealed that, during stable stratification, pressure transport plays an increasingly important role in supplying the canopy region with TKE.
机译:针对大范围的热稳定性等级,执行了许多大涡模拟(LES)来计算水平均质森林冠层上的气流。首次也显示了稳定分层冠层的LES结果。模拟结果与最近在瑞典东南部一片松树林上的实地测量结果相比具有优势。发现简单的热源模型可以充分发挥作用,并产生通常在现场稳定条件下观察到的冠层内部热通量曲线。证据表明,在稳定分层的情况下,冠层树干空间中存在一层不稳定的分层空气。在稳定的条件下,要强调次级风速最大值的重要性。对湍流动能(TKE)预算方程的研究表明,在稳定分层过程中,压力传输在为冠层区域提供TKE方面起着越来越重要的作用。

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