地基激光测风雷达的光束扫描及风场反演
The Beam Scanning and inversion method for detecting wind by lidar
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摘要: 激光测风雷达通过多普勒频移来确定激光束视线方向上的大气风场的速度矢量。由这些测得的矢量可反演大气风场群速的速度矢量。在本文中,我们将讨论利用单一LDV系统,激光束的扫描方式采用圆锥扫描,在扫描圆锥的垂直截面上取四个正交点上的多普勒风速矢量。通过这四个矢量,利用空间解析几何的知识,最终推导出观测视场上风场的水平和垂直方向的矢量分量。Abstract: Utilizing lidar to obtain the wind velocity along the line of sight by Doppler shift, then inverting these velocity vectors to real atmosphere wind group speed is a very important purpose of lidar. In this paper, we will describe the technique which utilize conical scanning known as velocity azimuth display based on single LDV system. The horizontal and vertical wind sect of the observed field can be gained by spatial analytic geometry’s operation and analysis on the four orthogonal points on the scanning cone’s vertical section.
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Key words:
- lidar /
- doppler shift /
- vector of wind field
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