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Aerosol lidar intercomparison in the framework of the EARLINET project. 3. Raman lidar algorithm for aerosol extinction, backscatter, and lidar ratio

机译:EARLINET项目框架中的气溶胶激光雷达比对。 3.拉曼激光雷达算法的气溶胶消光,反向散射和激光雷达比率

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An intercomparison of the algorithms used to retrieve aerosol extinction and backscatter starting from Raman lidar signals has been performed by 11 groups of lidar scientists involved in the European Aerosol Research Lidar Network (EARLINET). This intercomparison is part of an extended quality assurance program performed on aerosol lidars in the EARLINET. Lidar instruments and aerosol backscatter algorithms were tested separately. The Raman lidar algorithms were tested by use of synthetic lidar data, simulated at 355, 532, 386, and 607 nm, with realistic experimental and atmospheric conditions taken into account. The intercomparison demonstrates that the data-handling procedures used by all the lidar groups provide satisfactory results. Extinction profiles show mean deviations from the correct solution within 10% in the planetary boundary layer (PBL), and backscatter profiles, retrieved by use of algorithms based on the combined Raman elastic-backscatter lidar technique, show mean deviations from solutions within 20% up to 2 km. The intercomparison was also carried out for the lidar ratio and produced profiles that show a mean deviation from the solution within 20% in the PBL. The mean value of this parameter was also calculated within a lofted aerosol layer at higher altitudes that is representative of typical layers related to special events such as Saharan dust outbreaks, forest fires, and volcanic eruptions. Here deviations were within 15%.
机译:由涉及欧洲气溶胶研究激光雷达网络(EARLINET)的11组激光雷达科学家对从拉曼激光雷达信号开始的用于恢复气溶胶消光和反向散射的算法进行了比较。这种比对是EARLINET中对气溶胶激光雷达执行的扩展质量保证程序的一部分。激光雷达仪器和气溶胶反向散射算法分别进行了测试。拉曼激光雷达算法是通过使用合成的激光雷达数据进行测试的,该数据在355、532、386和607 nm进行了模拟,并考虑了实际的实验和大气条件。对比表明,所有激光雷达组使用的数据处理程序均提供令人满意的结果。消光剖面显示了行星边界层(PBL)中距正确解的10%以内的平均偏差,而反向散射剖面(通过使用基于拉曼弹性后向散射激光雷达组合技术的算法获得)显示了距解决方案的均偏差在20%以内至2公里。还对激光雷达比率进行了比较,并得出了一些轮廓,这些轮廓显示出在PBL中与溶液的平均偏差在20%以内。此参数的平均值也是在较高海拔的浮层气溶胶层中计算得出的,该层代表了与特殊事件(如撒哈拉粉尘暴发,森林火灾和火山喷发)相关的典型层。在这里,偏差在15%以内。

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