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A New Method for Retrieving Equivalent Cloud Base Height and Equivalent Emissivity by Using Ground-based Highresolution Infrared Radiance

机译:一种使用基于地面的高级别红外线辐射检索等效云基高度和等效发射率的新方法

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Based on the ground-based high-resolution infrared radiances observed by the Atmospheric Emitted Radiance Interferometer (AERI), a new method is proposed to identify the clear sky. Meanwhile, we also develop the new algorithms for retrieving the zenith equivalent cloud base height (CBH_e) and the equivalent emissivity (ε_e), respectively. The retrieval results in Shouxian indicate that the differences between the CBHe and observational cloud base height (CBH) are much smaller for thick low cloud, and increase with the increasing CBH. The average ε_e for the low, middle, and high cloud is 0.967, 0.781, and 0.616 for the 50 cases, respectively. It decreases with the increasing CBH. The new methods will be useful for studying the role of cloud in the radiation budget in the window region and cloud parameterizations in the climate model.
机译:基于由大气发射光线干涉仪(AERI)观察到的基于地基的高分辨率红外线,提出了一种新方法来识别晴朗的天空。同时,我们还开发了用于检索Zenith等效云基高(CBH_E)和等效发射率(ε_E)的新算法。 Shouxian的检索结果表明,CBHE和观察云基高度(CBH)之间的差异对于厚的低云的差异远小得多,并且随着CBH的增加而增加。 50例分别为0.967,0.781和0.616的平均Ε_E分别为0.967,0.781和0.616。它随着CBH的增加而降低。新方法对于研究窗口区域和气候模型中的云参数化的辐射预算中的作用将是有用的。

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