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首页> 外文期刊>Annales Geophysicae >Photon path length distributions for cloudy skies – oxygen A-Band measurements and model calculations
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Photon path length distributions for cloudy skies – oxygen A-Band measurements and model calculations

机译:多云天空的光子路径长度分布–氧气A波段测量和模型计算

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This paper addresses the statistics underlying cloudy sky radiative transfer (RT) by inspection of the distribution of the path lengths of solar photons. Recent studies indicate that this approach is promising, since it might reveal characteristics about the diffusion process underlying atmospheric radiative transfer (Pfeilsticker, 1999). Moreover, it uses an observable that is directly related to the atmospheric absorption and, therefore, of climatic relevance. However, these studies are based largely on the accuracy of the measurement of the photon path length distribution (PPD). This paper presents a refined analysis method based on high resolution spectroscopy of the oxygen A-band. The method is validated by Monte Carlo simulation atmospheric spectra. Additionally, a new method to measure the effective optical thickness of cloud layers, based on fitting the measured differential transmissions with a 1-dimensional (discrete ordinate) RT model, is presented. These methods are applied to measurements conducted during the cloud radar inter-comparison campaign CLARE’98, which supplied detailed cloud structure information, required for the further analysis. For some exemplary cases, measured path length distributions and optical thicknesses are presented and backed by detailed RT model calculations. For all cases, reasonable PPDs can be retrieved and the effects of the vertical cloud structure are found. The inferred cloud optical thicknesses are in agreement with liquid water path measurements. Key words. Meteorology and atmospheric dynamics (radiative processes; instruments and techniques)
机译:本文通过检查太阳光子路径长度的分布来解决多云辐射传输(RT)的基础统计问题。最近的研究表明,这种方法是有希望的,因为它可能揭示大气辐射传递背后的扩散过程的特征(Pfeilsticker,1999)。此外,它使用的观测值与大气吸收直接相关,因此与气候相关。但是,这些研究主要基于光子路径长度分布(PPD)的测量精度。本文提出了一种基于高分辨率氧谱的高分辨率分析方法。该方法通过蒙特卡罗模拟大气光谱验证。此外,提出了一种新的方法来测量云层的有效光学厚度,该方法基于将测得的差分透射率与一维(离散)RT模型拟合。这些方法适用于在云雷达比对活动CLARE’98期间进行的测量,该活动提供了进一步分析所需的详细云结构信息。对于某些示例性情况,将显示测量的路径长度分布和光学厚度,并通过详细的RT模型计算提供支持。对于所有情况,都可以获取合理的PPD并找到垂直云结构的影响。推断的云的光学厚度与液态水路径的测量结果一致。 关键词。 气象和大气动力学(辐射过程;仪器和技术)

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