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大气后向散射比对风速测量的影响

Effect of atmospheric back-scattering ratio on measurement of wind velocity
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摘要 采用同时测量Rayleigh散射和Mie散射混合信号的多普勒频移的单边缘技术,探测低空中(<12km)的大气风速。由于大气后向散射比Rb值的变化,导致测量结果有很大的误差。详细分析了Rb值的变化对风速测量灵敏度及测量结果的影响,并做出了在不同Rb值情况下的风速测量校正曲线。结果表明随着Rb值的增大,风速测量灵敏度有升高的趋势;随着Rb值偏差的增大,测量的风速误差有增大的趋势;同时,在相同的Rb值偏差情况下,随着径向风速的增大,测量的风速误差也有相应的增大。 The single-edge technique measuring Doppler shift of Rayleigh-scattering and Mie-scattering simultaneously is presented. The method is used to detect atmospheric wind velocity at low altitude(<12 km). The error of the measurement caused by the atmospheric back-scattering ratio R_b can't be ignored. The measurement sensitivity and results are analyzed. The calibrated curve of wind velocity measurement was calculated under different value of R_b. The results show that the sensitivity tends to increase along with the increase of R_b and the error of measurement increases along with the deviation of R_b. At the same time, the measuremental error tends to increase with the augment of the radial wind velocity under the same deviation of R_b.
出处 《强激光与粒子束》 EI CAS CSCD 北大核心 2005年第6期837-840,共4页 High Power Laser and Particle Beams
关键词 激光雷达 Rayleigh散射 MIE散射 大气后向散射比 风速 Lidar Rayleigh-scattering Mie-scattering Atmospheric back-scattering ratio Wind velocity
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