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Numerical simulation including model validation of wind flow in alpine terrain in eastern Switzerland

机译:数值模拟,包括瑞士东部高山地形中风流的模型验证

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A model for the simulation of wind flow in alpine terrain is presented. The model is based on the Reynolds averaged Navier-Stokes equations using a κ-ε turbulence model. Additional terms are implemented in the energy equation to describe dry adiabatic cooling in the atmosphere. The orography and flora of the Earth's surface are described by high resolution data from swisstopo. Boundary and initial conditions are based on mesoscale simulation data from the COSMO-2 weather model of the MeteoSwiss. Various nestings with different grid resolutions are used to simulate wind flow in the region between Vaduz and Landquart located in Liechtenstein and Switzerland, respectively. The model is validated with light detecting and ranging (LIDAR) and cup anemometer velocity measurements from three locations for a specific foehn weather situation. Finally, the model is used to get a first indication of potential locations for the placement of wind turbines.
机译:提出了一种模拟高山地形气流的模型。该模型基于使用κ-ε湍流模型的雷诺平均Navier-Stokes方程。在能量方程式中使用了其他术语来描述大气中的干燥绝热冷却。 swisstopo的高分辨率数据描述了地球表面的地形和植物区系。边界条件和初始条件基于来自MeteoSwiss COSMO-2天气模型的中尺度模拟数据。使用具有不同网格分辨率的各种嵌套来模拟分别位于列支敦士登和瑞士的瓦杜兹(Vaduz)和兰夸特(Landquart)之间的区域中的风流。该模型已针对特定的foehn天气情况从三个位置进行了光检测和测距(LIDAR)以及杯型风速计速度测量,从而进行了验证。最后,该模型用于获得风力涡轮机放置位置的第一个指示。

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