小光学数据集条件下正则化反演反演大气粒子物理性质

D. Müller, A. Ansmann, U. Wandinger, D. Althausen
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引用次数: 0

摘要

大气气溶胶虽然只占地球大气的一小部分,但在许多大气过程中起着重要作用。由于它们对地球的辐射收支、空气质量、云和降水以及对流层和平流层的化学有明显的影响,因此有必要收集关于它们的光学和物理性质的详细资料。该研究所的多波长激光雷达和拉曼激光雷达在0.355 ~ 1.064 μm的垂直波长范围内提供了6个后向散射系数和2个消光系数的光学粒子信息。为了从给定的光学信息中检索物理性质,专门设计了一种使用正则化反演方法的数据评估算法。物理参数可以用粒径分布、平均粒径、有效半径、体积、表面积、粒子数浓度以及复折射率等来描述。由于关于粒子性质的先验信息很少,加上光学信息数量少,另外还包括较大的测量误差,因此主要的重点是均值的检索。为了在这些困难的条件下控制正则化的质量,使用了广义交叉验证的方法,因为它不需要了解潜在的测量误差,也不需要了解粒度分布的特定形状。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Retrieval of Physical Properties of Atmospheric Particles by Inversion via Regularization in the Limit of a Small Optical Data Set
Atmospheric aerosols, although only a minor constituent of the earth’s atmosphere, play an important role in many atmospheric processes. Due to their appreciable influence on the earth’s radiation budget, air quality, clouds and precipitation as well as the chemistry of the troposphere and stratosphere it is necessary to gather detailed information on their optical and physical properties. A multiple-wavelength lidar as well as a Raman lidar at the Institute provide optical particle information in terms of six backscatter coefficients and two extinction coefficients in the wavelength range from 0.355 to 1.064 μm on a vertical scale. A data-evaluation algorithm that uses the method of inversion via regularization has been specifically designed to retrieve physical properties from the given optical information. The physical parameters can be described by, e.g., the particle size distributions, the mean sizes derived from it, like the effective radius, the volume, surface-area, and number concentrations as well as the complex refractive index. Due to the low amount of available a priori information on the particle properties in combination with the small number of optical information that additionally include large measurement errors the main focus had been on the retrieval of the mean values. To control the quality of the regularization under these difficult conditions the method of generalized cross-validation is used as it does not require the knowledge of the underlying measurement errors nor the knowledge of the specific shape of the particle size distributions.
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