Ansmann Albert, Wandinger Ulla, Le Rille Olivier, Lajas Dulce, Straume Anne Grete
Leibniz Institute for Tropospheric Research, Leipzig, Germany.
Appl Opt. 2007 Sep 10;46(26):6606-22. doi: 10.1364/ao.46.006606.
The European Space Agency will launch the Atmospheric Laser Doppler Instrument (ALADIN) for global wind profile observations in the near future. The potential of ALADIN to measure the optical properties of aerosol and cirrus, as well, is investigated based on simulations. A comprehensive data analysis scheme is developed that includes (a) the correction of Doppler-shifted particle backscatter interference in the molecular backscatter channels (cross-talk effect), (b) a procedure that allows us to check the quality of the cross-talk correction, and (c) the procedures for the independent retrieval of profiles of the volume extinction and backscatter coefficients of particles considering the height-dependent ALADIN signal resolution. The error analysis shows that the particle backscatter and extinction coefficients, and the corresponding extinction-to-backscatter ratio (lidar ratio), can be obtained with an overall (systematic+statistical) error of 10%-15%, 15%-30%, and 20%-35%, respectively, in tropospheric aerosol and dust layers with extinction values from 50 to 200 Mm(-1); 700-shot averaging (50 km horizontal resolution) is required. Vertical signal resolution is 500 m in the lower troposphere and 1000 m in the free troposphere. In cirrus characterized by extinction coefficients of 200 Mm(-1) and an optical depth of >0.2, backscatter coefficients, optical depth, and column lidar ratios can be obtained with 25%-35% relative uncertainty and a horizontal resolution of 10 km (140 shots). In the stratosphere, only the backscatter coefficient of aerosol layers and polar stratospheric clouds can be retrieved with an acceptable uncertainty of 15%-30%. Vertical resolution is 2000 m.
欧洲航天局将在不久的将来发射大气激光多普勒仪(ALADIN)用于全球风廓线观测。基于模拟研究了ALADIN测量气溶胶和卷云光学特性的潜力。开发了一种综合数据分析方案,该方案包括:(a)校正分子后向散射通道中多普勒频移粒子后向散射干扰(串扰效应);(b)一种可让我们检查串扰校正质量的程序;(c)考虑与高度相关的ALADIN信号分辨率独立反演粒子体积消光系数和后向散射系数廓线的程序。误差分析表明,在对流层气溶胶和尘埃层中,消光值为50至200Mm⁻¹时,粒子后向散射系数和消光系数以及相应的消光与后向散射比(激光雷达比)的总体(系统误差+统计误差)分别可达10%-15%、15%-30%和20%-35%;需要700次测量平均(水平分辨率50km)。对流层下部垂直信号分辨率为500m,自由对流层为1000m。在卷云的消光系数为200Mm⁻¹且光学厚度>0.2的情况下,后向散射系数、光学厚度和柱状激光雷达比可在相对不确定度为25%-35%且水平分辨率为10km(140次测量)的情况下获得。在平流层中,仅气溶胶层和极地平流层云的后向散射系数可在15%-30%的可接受不确定度下反演得到。垂直分辨率为2000m。