On the role of the method of measuring the background signal in the lidar measurements of the upper atmosphere

机译：关于背景信号测量方法在高空激光雷达测量中的作用

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The paprr presents the results of a lidar study of the atmosphere in the altitude region of 100-400 km, obtained at the lidar station of Kamchatka. The development of methods for lidar measurements and signal processing is discussed. The method that takes into account the technique to measure the background signal is described. These tools allow the authors to include the atmosphere into the altitude region investigated by the lidar method. The results of the investigation of the backscattering lidar signal from the altitude region of 100-400 km caused by the resonance scattering on exited components of upper atmosphere are discussed.

机译：这篇论文介绍了在堪察加激光雷达站获得的100-400 km海拔地区的激光雷达研究结果。讨论了激光雷达测量和信号处理方法的发展。描述了考虑到测量背景信号的技术的方法。这些工具使作者能够将大气纳入通过激光雷达法研究的海拔区域。讨论了对高层大气出口分量的共振散射引起的100-400 km高度区域后向散射激光雷达信号的研究结果。

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《International symposium on atmospheric and ocean optics: atmospheric physics》|2017年|1046677.1-1046677.5|共5页
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Vasily V. Bychkov; Andrey S. Perezhogin; Ilya X. Seredkin; Boris M. Shevtsov;
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atmosphere; lidar; stratosphere; mesosphere; scattering; sounding;

机译：大气层;激光雷达平流层中层散射;听起来;

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2. The interdependence of continental warm cloud properties derived from unexploited solar background signals in ground-based lidar measurements [J] . J. C. Chiu, J. A. Holmes, R. J. Hogan, Atmospheric chemistry and physics . 2014,第16期

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3. The interdependence of continental warm cloud properties derived from unexploited solar background signals in ground-based lidar measurements [J] . Chiu J. C., Holmes J. A., Hogan R. J., Atmospheric Chemistry and Physics Discussions . 2014,第16期

机译：在基于地面的激光雷达测量中源于未开发的太阳能背景信号的欧式温暖云属性的相互依存
4. On the role of the method of measuring the background signal in the lidar measurements of the upper atmosphere [C] . Vasily V. Bychkov, Andrey S. Perezhogin, Ilya N. Seredkin, International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics . 2017

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机译：利用激光雷达精确测量去极化率的三信号法

On the role of the method of measuring the background signal in the lidar measurements of the upper atmosphere

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