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Measurements and Modelling of the Wind Speed Profile in the Marine Atmospheric Boundary Layer

机译:海洋大气边界层风速剖面的测量和建模

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We present measurements from 2006 of the marine wind speed profile at a site located 18 km from the west coast of Denmark in the North Sea. Measurements from mast-mounted cup anemometers up to a height of 45 m are extended to 161 m using LiDAR observations. Atmospheric turbulent flux measurements performed in 2004 with a sonic anemometer are compared to a bulk Richardson number formulation of the atmospheric stability. This is used to classify the LiDAR/cup wind speed profiles into atmospheric stability classes. The observations are compared to a simplified model for the wind speed profile that accounts for the effect of the boundary-layer height. For unstable and neutral atmospheric conditions the boundary-layer height could be neglected, whereas for stable conditions it is comparable to the measuring heights and therefore essential to include. It is interesting to note that, although it is derived from a different physical approach, the simplified wind speed profile conforms to the traditional expressions of the surface layer when the effect of the boundary-layer height is neglected.
机译:我们介绍了自2006年以来在距丹麦西海岸18公里的北海一个站点中海洋风速剖面的测量值。使用LiDAR观测值,将安装在桅杆式风速计上的高度高达45 m的测量值扩展到161 m。将2004年使用声速风速计进行的大气湍流通量测量与大气稳定性的总体Richardson数公式进行了比较。这用于将LiDAR /杯风速曲线分类为大气稳定性类别。将观察结果与简化的风速剖面模型进行比较,该模型考虑了边界层高度的影响。对于不稳定和中性的大气条件,边界层的高度可以忽略,而对于稳定条件,它可以与测量高度相比,因此必须包括在内。有趣的是,尽管忽略了边界层高度的影响,但简化的风速曲线虽然源自不同的物理方法,但仍符合表层的传统表达式。

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