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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

摘要

The extinction-to-backscatter ratio (S(sub 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 Sa for the Cloud and Aerosol Lidar and Infrared Pathfinder Spaceborne Observations (CALIPSO) lidar. S(sub 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(sub a) is computed directly from the integrated backscatter and transmittance. In all other cases, the CALIPSO observables: the depolarization ratio, delta, the layer integrated attenuated backscatter, beta, and the mean layer total attenuated color ratio, gamma, 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(sub 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(sub a))是确定气溶胶消光以及随后由激光雷达背向散射测量得出的光学深度的重要参数。我们概述了用于确定云,气溶胶激光雷达和红外探路者星载观测(CALIPSO)激光雷达的Sa的算法。 CALIPSO激光雷达的S(sub 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。每当遇到合适的放样层时,就直接根据积分的反向散射和透射率来计算S(sub a)。在所有其他情况下,可观察到CALIPSO:使用去极化率delta,层积分后向散射衰减系数beta和平均层总衰减后的色彩比率γ以及表面类型,以帮助进行气溶胶分型。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(sub 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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