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Simultaneous Raman and Mie-Rayleigh lidar measurement in the lower troposphere

机译:对流层下层同时进行拉曼和Mie-Rayleigh激光雷达测量

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摘要

A lidar system capable of simultaneous measurement of Raman and Mie-Rayleigh scattering was constructed, and used for measurement of O_3, water vapor, and aerosols in the lower troposphere. O_3 concentration measurement was performed by differential absorption of N_2 and O_2 Raman scattering signals with the lidar transmitter operating at 280.0 nm, and also by differential absorption of Mie-Rayleigh scattering and of N_2 Raman scattering with the transmitter operating at 279.5 nm and 280.5 nm on alternate pulses. Water vapor profiles were obtained as the mix ing ratio relative to N_2 using the N_2 and H_2O Raman scattering signals with the lidar transmitter operating at 280.0 nm. Simultaneous measurement of H_2O Raman scattering and Mie scattering over a continuous period of about 13 hours showed that the lidar system can identify uncondensed water vapor and condensed water vapor by comparison of temporal and spatial variations of the water vapor mixing ratio and of the Mie backscattering coefficient.
机译:构造了能够同时测量拉曼散射和米-瑞利散射的激光雷达系统,并将其用于测量对流层下层的O_3,水蒸气和气溶胶。 O_3浓度测量是通过在280.0 nm激光雷达发射器上差分吸收N_2和O_2拉曼散射信号,以及通过在279.5 nm和280.5 nm发射器上发射的Mie-Rayleigh散射和N_2 Raman散射差分吸收来进行的。交替脉冲。使用N_2和H_2O拉曼散射信号,并在激光雷达发射器工作于280.0 nm的情况下,获得相对于N_2的混合比的水蒸气剖面。在大约13个小时的连续时间内对H_2O拉曼散射和Mie散射的同时测量表明,激光雷达系统可以通过比较水蒸汽混合比和Mie后向散射系数的时空变化来识别未冷凝的水蒸气和冷凝的水蒸气。 。

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