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首页> 外文期刊>Journal of Quantitative Spectroscopy & Radiative Transfer >An iterative calculation to derive extinction-to-backscatter ratio based on lidar measurements
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An iterative calculation to derive extinction-to-backscatter ratio based on lidar measurements

机译:基于激光雷达测量值得出消光与后向散射比的迭代计算

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The aerosol optical thickness (AOT) is an important parameter for understanding the radiative impact of aerosols. AOT based on lidar measurements is often limited by its finite detection range. In this paper, we have reported a method of fitting and iterative calculation to derive the extinction profile of background aerosols from 0 to 30 krn at 532 nm, which is virtually the AOT of the entire atmosphere. The mean extinction derived from this method at the ground level tallies with visibility measurement and it is also consistent with the sun-photometer data, within experimental error. These data have been further treated to study the dust cases. For most of the cases, transmission losses were determined to estimate the extinction as well as lidar ratio. The result of the analysis shows that for background aerosols, a mean lidar ratio of 47 +/- 15sr was found. For dust layers, a mean lidar ratio of 44 +/- 19sr and an optical thickness of 0.53 +/- 0.49 were determined at 532 nm. (c) 2007 Elsevier Ltd. All rights reserved.
机译:气溶胶光学厚度(AOT)是了解气溶胶辐射影响的重要参数。基于激光雷达测量的AOT通常受其有限的检测范围限制。在本文中,我们报告了一种拟合和迭代计算的方法,可得出背景气溶胶在532 nm处从0到30 krn的消光曲线,这实际上是整个大气的AOT。这种方法在地面上的平均消光与能见度测量相符,并且在实验误差范围内也与太阳光度计数据一致。这些数据已被进一步处理以研究尘埃事件。对于大多数情况,确定传输损耗以估计消光以及激光雷达比。分析结果表明,对于背景气溶胶,平均激光雷达比为47 +/- 15sr。对于灰尘层,在532 nm处测得的平均激光雷达比为44 +/- 19sr,光学厚度为0.53 +/- 0.49。 (c)2007 Elsevier Ltd.保留所有权利。

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