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Selection algorithm for the CALIPSO lidar aerosol extinction-to-backscatter ratio

机译:CALIPSO激光雷达消光与后向散射比的选择算法

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摘要

The extinction-to-backscatter ratio (S_a) is an important parameter used in the determination of the aerosol extinction and subsequently the optical depth from lidar backscatter measurements. We outline the algorithm used to determine S_a for the Cloud and Aerosol Lidar and Infrared Pathfinder Spaceborne Observations (CALIPSO) lidar. S_a for the CALIPSO lidar will either be selected from a look-up table or calculated using the lidar measurements depending on the characteristics of aerosol layer. Whenever suitable lofted layers are encountered, S_a is computed directly from the integrated backscatter and transmittance. In all other cases, the CALIPSO observables: the depolarization ratio, δ, the layer integrated attenuated backscatter, β', and the mean layer total attenuated color ratio, γ, together with the surface type, are used to aid in aerosol typing. Once the type is identified, a look-up-table developed primarily from worldwide observations, is used to determine the S_a value. The CALIPSO aerosol models include desert dust, biomass burning, background, polluted continental, polluted dust, and marine aerosols.
机译:消光与背向散射比(S_a)是确定气溶胶消光以及随后从激光雷达背向散射测量确定光学深度时使用的重要参数。我们概述了用于确定云和气溶胶激光雷达和红外探路者星载观测(CALIPSO)激光雷达的S_a的算法。 CALIPSO激光雷达的S_a可以从查询表中选择,也可以根据气溶胶层的特性使用激光雷达测量来计算。只要遇到合适的放样层,就直接根据积分的反向散射和透射率来计算S_a。在所有其他情况下,可观察到CALIPSO:使用去极化率δ,层积分后向散射衰减β'和平均层总衰减色率γ与表面类型一起用于气溶胶分型。一旦确定了类型,就会使用主要从全球范围内观察得出的查询表来确定S_a值。 CALIPSO气溶胶模型包括沙漠尘埃,生物质燃烧,背景,被污染的大陆,被污染的尘埃和海洋气溶胶。

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