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Validation of the Dust Layer Structure over the Taklimakan Desert, China by the CALIOP Space-Borne Lidar Using Ground-Based Lidar

机译:塔利玛干沙漠中中国沙尘层结构的CALIOP地面波激光雷达的CALIOP验证

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References(21) Cited-By(1) Supplementary materials(1) A ground-based lidar observation was carried out in the northwest of China to validate the space-borne lidar CALIOP on 23 March 2009. Combining backscatter profiles of the ground-based lidar and CALIOP, lidar ratio (extinction to backscattering ratio) was retrieved for 532 nm and 1064 nm wavelengths by using performance function that minimizing the difference between the ground-based lidar and CALIOP for backscattering coefficient. The correlation coefficients between them were 0.98 for 532 nm and 0.95 1064 nm, respectively. Using the retrieved lidar ratio, the color ratio and aerosol optical depth (AOD) were calculated. The observed aerosols and clouds were classified into three groups (boundary layer dust, free tropospheric aerosol and cirrus cloud) according to a relationship between color ratio and 532 nm-backscattering coefficient.
机译:参考文献(21)引用了(1)补充材料(1)2009年3月23日,在中国西北部进行了地面激光雷达观测,以验证星载激光雷达CALIOP。结合地面激光雷达的反向散射剖面激光雷达和CALIOP,通过使用性能函数检索了532 nm和1064 nm波长的激光雷达比(消光与后向散射比),该函数使基于地面的激光雷达和CALIOP之间的后向散射系数之间的差异最小。它们之间的相关系数对于532 nm分别为0.98和0.95 1064 nm。使用检索到的激光雷达比,计算色比和气溶胶光学深度(AOD)。根据色比与532 nm后向散射系数之间的关系,将观测到的气溶胶和云划分为三类(边界层粉尘,对流层自由气溶胶和卷云)。

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