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Cloud Base Height and Effective Cloud Emissivity Retrieval with Ground-Based Infrared Interferometer

机译:地基红外干涉仪的云底高度和有效的云发射率反演

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摘要

Based on ground-based Atmospheric Emitted Radiance Interferometer (AERI) observations in Shouxian, Anhui province, China, the authors retrieve the cloud base height (CBH) and effective cloud emissivity by using the minimum root-mean-square difference method. This method was originally developed for satellite remote sensing. The high-temporal-resolution retrieval results can depict the trivial variations of the zenith clouds continu- ously. The retrieval results are evaluated by comparing them with observations by the cloud radar. The compari- son shows that the retrieval bias is smaller for the middle and low cloud, especially for the opaque cloud. When two layers of clouds exist, the retrieval results reflect the weighting radiative contribution of the multi-layer cloud. The retrieval accuracy is affected by uncertainties of the AERI radiances and sounding profiles, in which the role of uncertainty in the temperature profile is dominant.
机译:基于中国安徽寿县的地面大气发射辐射干涉仪(AERI)观测,作者使用最小均方差法检索了云底高度(CBH)和有效云发射率。此方法最初是为卫星遥感开发的。高温分辨率的检索结果可以连续描述天顶云的微小变化。通过将检索结果与云雷达的观测结果进行比较来评估检索结果。比较表明,对于中低云,特别是对于不透明云,检索偏向较小。当存在两层云时,检索结果反映了多层云的加权辐射贡献。检索精度受AERI辐射和测深曲线的不确定性影响,其中温度曲线中不确定性的作用占主导。

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