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Doppler Lidar-Based Wind-Profile Measurement System for Offshore Wind-Energy and Other Marine Boundary Layer Applications

机译:基于多普勒激光雷达的风廓线测量系统,用于海上风能和其他海洋边界层应用

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Accurate measurement of wind speed profiles aloft in the marine boundary layer is a difficult challenge. The development of offshore wind energy requires accurate information on wind speeds above the surface at least at the levels occupied by turbine blades. Few measured data are available at these heights, and the temporal and spatial behavior of near-surface winds is often unrepresentative of that at the required heights. As a consequence, numerical model data, another potential source of information, are essentially unverified at these levels of the atmosphere. In this paper, a motion-compensated, high-resolution Doppler lidar-based wind measurement system that is capable of providing needed information on offshore winds at several heights is described. The system has been evaluated and verified in several ways. A sampling of data from the 2004 New England Air Quality Study shows the kind of analyses and information available. Examples include time-height cross sections, time series, profiles, and distributions of quantities such as winds and shear. These analyses show that there is strong spatial and temporal variability associated with the wind field in the marine boundary layer. Winds near the coast show diurnal variations, and frequent occurrences of low-level jets are evident, especially during nocturnal periods. Persistent patterns of spatial variability in the flow field that are due to coastal irregularities should be of particular concern for wind-energy planning, because they affect the representativeness of fixed-location measurements and imply that some areas would be favored for wind-energy production whereas others would not.
机译:在海洋边界层高空准确测量风速分布是一项艰巨的挑战。海上风能的发展需要至少在涡轮叶片占据的水平面上有关地面以上风速的准确信息。在这些高度上几乎没有可用的测量数据,并且近地表风的时空行为通常不能代表所需高度上的情况。因此,数值模型数据(另一种潜在的信息来源)在大气层的这些高度上基本上未被验证。在本文中,描述了一种基于运动补偿的高分辨率多普勒激光雷达的风测量系统,该系统能够提供有关几个高度的海上风的所需信息。该系统已通过多种方式进行了评估和验证。 2004年《新英格兰空气质量研究》的数据样本显示了这种分析和可用信息。示例包括时间高度截面,时间序列,轮廓以及诸如风和切变之类的数量分布。这些分析表明,海洋边界层中的风场具有很强的时空变异性。海岸附近的风表现出昼夜变化,并且低空急流的频繁发生是明显的,尤其是在夜间。沿海地区的不规则性引起的流场永久性空间变化模式应特别关注风能规划,因为它们会影响固定位置测量的代表性,并暗示某些地区将有利于风能生产,而其他人不会。

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