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Retrieval of Vertical Profile of Cirrus Cloud Effective Particle Size Using Reflected Line Spectra in 1.38?μm Band

机译:使用反射线谱在1.38Ω·μm频段中检索卷云有效粒度的垂直轮廓的垂直轮廓

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This paper presents a new retrieval method for inferring the vertical profile of cirrus cloud effective particle size by using solar reflected line spectra in the 1.38‐μm band. The retrieval method is based on the maximum‐photon penetration principle coupled with the constrained linear inversion. This approach takes advantage of the vertical stratification of cirrus cloud effective particle size as well as absorption lines of water vapor of different intensity, which contain rich information on the vertical structure of cloud particle size. Reflected radiances at different wavenumbers provide the effective‐size information at different heights within cirrus associated with photon different penetration depths. Assuming a vertical profile of effective size monotonically decreasing toward cloud top and using results based on “exact” radiative transfer computations, we perform retrieval of the effective size for a number of model cirrus to check for algorithm accuracy. The retrieved profile of effective size is close to the model profile for cirrus optical depth less than about eight with an uncertainty range of 2.2–4.2?μm. In addition, we further carry out a sensitivity study involving the retrieved effective size in connection with different water vapor profiles and demonstrate that the difference from the model is only several percent except for the cloud top if an appropriate wavenumber set is selected. The results from this study suggest that the present method can be applied to realistic remote sensing of the vertical profile of cirrus cloud particle size.
机译:本文介绍了一种新的检索方法,用于推断在1.38-μm波段中的太阳反射线谱推断螺旋云有效粒度的垂直轮廓。检索方法基于与约束线性反转耦合的最大光子渗透原理。这种方法利用岩云有效粒度的垂直分层以及不同强度的水蒸气吸收线,其含有关于云粒径的垂直结构的丰富信息。在不同的波兰管的反射辐射提供了与光子不同穿透深度相关的卷曲内不同高度的有效尺寸信息。假设有效尺寸的垂直轮廓单调地向云顶部和基于“精确”辐射转移计算的结果,我们执行多个模型循环的有效尺寸的检索,以检查算法精度。检索到的有效尺寸的轮廓接近螺旋光学深度小于约8的模型轮廓,不确定范围为2.2-4.2≤μm。此外,我们还进行敏感性研究,涉及与不同的水蒸气分布有关的检索有效尺寸,并证明与模型的差异仅为云顶部,如果选择了合适的波数集,则云顶部的差异是几个百分点。本研究的结果表明,本方法可以应用于岩体云粒径垂直轮廓的逼真遥感。

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