A Simplified Algorithm to the Atmospheric Transmittance

Shan Chen, Ji-yin Sun
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引用次数: 1

Abstract

It is very complex that the infrared radiation's actual transmission process through earth's atmosphere. There is interaction between radiation and atmospheric component. The radiation transmittance will be weakened because of the absorption and the scattering. The atmospheric transmittance is an important parameter to measure the attenuation. This paper summarizes the infrared radiation's transmission process in atmosphere, studies the computation method of atmospheric transmittance, analyzes the absorption attenuation of the atmospheric gas such as steam and carbon dioxide, the scattering attenuation and the attenuation caused by meteorological condition, infers the computation method of the atmospheric equivalent path, and gives the atmospheric transmittance simplified algorithm. Finally this paper gives the atmospheric transmittance computation result under given meteorological condition, also gives the contrast curve with LOWTRAN7.0. The algorithm has certain reference value in the project application. The problem that the infrared radiation transmits in the atmosphere is always paid attention by the designers who deal with the photoelectricity measurement system and the researchers who deal with the radiation transmission in the earth atmosphere. There is more and more attached importance to the research of the atmospheric transmission model. There are many studies relating to the atmospheric transmission characteristic of infrared radiation, such as the object infrared detection, the navigation, the communication, the earth resource distance survey, etc. Generally there are three atmospheric radiation transmission models such as LOWTRAN, MODTRAN and FASCODE. These application softwares are developed by Air Force Geophysics Laboratory of America (AFGL) according to different application purpose. But it is complex to use these softwares by many project personnel. This paper gives a kind of atmospheric transmittance simplified algorithm.
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大气透射率的一种简化算法
红外辐射在地球大气中的实际传输过程是非常复杂的。辐射与大气成分之间存在相互作用。由于吸收和散射,辐射透过率会降低。大气透过率是测量衰减的重要参数。本文总结了红外辐射在大气中的传输过程,研究了大气透过率的计算方法,分析了大气中蒸汽、二氧化碳等气体的吸收衰减、散射衰减和气象条件引起的衰减,推导了大气等效路径的计算方法,给出了大气透过率的简化算法。最后给出了给定气象条件下的大气透过率计算结果,并给出了与LOWTRAN7.0的对比曲线。该算法在工程应用中具有一定的参考价值。红外辐射在大气中的传输问题一直是从事光电测量系统设计人员和从事地球大气辐射传输研究人员所关注的问题。大气传输模式的研究越来越受到重视。红外辐射大气传输特性的研究有很多,如目标红外探测、导航、通信、地球资源距离测量等。大气辐射传输模式一般有LOWTRAN、MODTRAN和FASCODE三种。这些应用软件是美国空军地球物理实验室(AFGL)根据不同的应用目的开发的。但是对于许多项目人员来说,使用这些软件是很复杂的。本文给出了一种大气透射率的简化算法。
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