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Wind speed measurements of Doppler-shifted absorption lines using two-beam interferometry

机译:使用两束干涉仪测量多普勒频移吸收线的风速

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Wind speed can be measured remotely, with varying degrees of success, using interferometry of Doppler-shifted optical spectra. Under favorable conditions, active systems using laser pulse backscatter are capable of high resolution; passive systems, which measure Doppler shifts of atmospheric emission lines in the mesosphere, have also been shown. Two-beam interferometry of Doppler-shifted absorption lines has not been previously investigated; we describe such an effort here. Even in a well-defined environment, measuring absorption line Doppler shifts requires overcoming several technical hurdles in order to obtain sensitivity to wind speeds on the order of 10 m/s. These hurdles include precise knowledge of the shape of the absorption line, tight, stable filtering, and understanding precisely how an interferometer phase should respond to a change in the absorption profile. We discuss the instrument design, a Michelson interferometer and Fabry-Perot filter, and include an analysis of how to choose the optimal optical path difference of the two beams for a given spectrum and filter. We discuss two beam interferometric measurements of emission line and absorption line Doppler shifts, and include an illustration of the effects of filtering on LIDAR Doppler interferometry. Finally, we discuss the construction and implementation of a Michelson interferometer used to measure Doppler shifts of oxygen absorption lines and present results obtained with 5 m/s wind speed measurement precision. Although the theoretical shot noise limited Doppler wind speed measurement of the system described can be less than 1 m/s, the instrument's resolution limit is dominated by residual filter instability. Application of absorption line interferometry to determine atmospheric wind speeds remains problematic.
机译:使用多普勒频移光谱的干涉仪,可以以不同的成功程度远程测量风速。在有利的条件下,使用激光脉冲反向散射的有源系统具有高分辨率。还显示了可测量中层大气发射线多普勒频移的无源系统。多普勒频移的吸收线的两光束干涉测量法以前没有研究过;我们在这里描述这样的努力。即使在定义明确的环境中,测量吸收线的多普勒频移也需要克服几个技术障碍,以便获得对风速约10 m / s的灵敏度。这些障碍包括对吸收线形状的精确了解,紧密,稳定的滤波,以及精确地理解干涉仪相位应如何响应吸收曲线的变化。我们讨论了仪器设计,迈克尔逊干涉仪和Fabry-Perot滤波器,并分析了如何针对给定的光谱和滤波器选择两条光束的最佳光程差。我们讨论了发射线和吸收线多普勒频移的两个光束干涉测量,并包括了对LIDAR多普勒干涉测量滤波效果的说明。最后,我们讨论了用于测量氧气吸收线的多普勒频移的迈克尔逊干涉仪的构造和实现,并给出了以5 m / s风速测量精度获得的结果。尽管所描述系统的理论上受散粒噪声限制的多普勒风速测量结果可能小于1 m / s,但仪器的分辨率极限仍受残余滤波器不稳定的影响。应用吸收线干涉测量法确定大气风速仍然是有问题的。

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