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后向散射辐射探测大气臭氧总量反演方法的改进
引用本文:江芳,王英鉴,王咏梅.后向散射辐射探测大气臭氧总量反演方法的改进[J].空间科学学报,2006,26(5):352-356.
作者姓名:江芳  王英鉴  王咏梅
作者单位:中国科学院空间技术与应用研究中心,北京,100080;中国科学院研究生院;中国科学院空间技术与应用研究中心,北京,100080
摘    要:以SBDART模式作为辐射传输计算模式,在各种大气气溶胶存在的情况下利用现有的大气后向散射反演大气臭氧总量的Version7方法,模拟计算得到各种气溶胶存在时的大气臭氧总量,并分析了反演结果误差产生的原因.进一步提出根据斜气柱臭氧总量sΩ0,选择不同连续波长区间测量得到的后向散射强度来对臭氧总量的初估值Ω0进行修正的方法.将得到的结果与Version7的进行比较,证明了新方法的有效性. 

关 键 词:大气臭氧总量  紫外后向散射  下垫面有效反照率  斜气柱臭氧总量
收稿时间:2005-10-16
修稿时间:2006-04-18

An Improvement on Retrieval Method of Total Ozone's Determination Using Backscattered Ultraviolet Earth Radiances' Measurements
JIANG Fang,WANG Yingjian,WANG Yongmei.An Improvement on Retrieval Method of Total Ozone's Determination Using Backscattered Ultraviolet Earth Radiances' Measurements[J].Chinese Journal of Space Science,2006,26(5):352-356.
Authors:JIANG Fang  WANG Yingjian  WANG Yongmei
Institution:1.Center for Space Science and Applied Research, Chinese Academy of Sciences, Beijing 1000802.Graduate School, Chinese Academy of Sciences
Abstract:Values of the total ozone content of an atmospheric column are estimated from the simulated measurements of the intensity of radiation backscattered by a horizontally homogeneous earth-atmosphere system by means of SBDART radiative transfer computation mode with atmo- sphere containing varions kinds of aerosols. The retrieval method used is the Version7 algorithm. When all kinds of aerosols are present in the atmosphere the retrieval error is analyzed and the main reason which brings the error is the assumption of the residues being linear at the properly chosen triplet of wavelengths. In the paper a method is introduced to correct the initial ozone estimate Ω0 using the intensity radiation backscattered measured at different continuous ultraviolet spectral region which is selected on the basis of the ozone slant column density sΩ0. At last the results obtained by the new method and Version7 algorithm are compared. The comparing result proves the new method's validity. 
Keywords:Total column ozone  Backscattered ultraviolet radiance  Effective surface reflectivity  Slant column ozone
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