首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Retrieval of vertical columns of sulfur dioxide from SCIAMACHY andOMI: Air mass factor algorithm development, validation, and erroranalysis
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Retrieval of vertical columns of sulfur dioxide from SCIAMACHY andOMI: Air mass factor algorithm development, validation, and erroranalysis

机译:从SCIAMACHY和OMI中检索垂直二氧化硫柱:空气质量因子算法的开发,验证和误差分析

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We develop an improved retrieval of sulfur dioxide (SO2) vertical columns from twosatellite instruments (SCIAMACHY and OMI) that measure ultraviolet solar backscatter.For each SCIAMACHY and OMI observation, a local air mass factor (AMF) algorithmconverts line-of-sight "slant" columns to vertical columns using altitude-dependent scattering weights computed with a radiative transfer model (LIDORT), weighted byrelative vertical SO2 profile (shape factor) determined locally with a global atmosphericchemistry model (GEOS-Chem). The scattering weights account for viewing geometry,surface albedo, cloud scattering, absorption by ozone, and scattering and absorption by aerosols. Absorption of radiation by mineral dust can reduce seasonal mean instrumentsensitivity by 50%. Mean SO2 shape factors simulated with GEOS-Chem and used in theAMF calculation are highly consistent with airborne in situ measurements (INTEX-Aand INTEX-B); differences would affect the retrieved SO2 columns by 10%. The retrievedvertical columns are validated with coincident airborne in situ measurements (INTEX-A,INTEX-B, and a campaign over east China). The annual mean AMF errors are estimatedto be 35-70% in polluted regions (e.g., East Asia and the eastern United States) andless than 10% over clear ocean regions. The overall SO2 error assessment is 45-80% foryearly averages over polluted regions. Seasonal mean SO2 columns retrieved fromSCIAMACHY and OMI for 2006 are significantly spatially correlated with those fromGEOS-Chem, in particular over the United States (r = 0.85 for SCIAMACHY and 0.82 forOMI). A sensitivity study confirms the sensitivity of SCIAMACHY and OMI toanthropogenic SO2 emissions.
机译:我们开发了一种改进的测量方法,可以从两个用于测量紫外线太阳反向散射的卫星仪器(SCIAMACHY和OMI)中检索二氧化硫(SO2)垂直柱。对于每个SCIAMACHY和OMI观测,本地空气质量因子(AMF)算法都可以将视线“倾斜” ”列到垂直列,使用通过辐射传输模型(LIDORT)计算的高度相关的散射权重,并通过使用全球大气化学模型(GEOS-Chem)局部确定的相对垂直SO2轮廓(形状因子)进行加权。散射权重包括观察几何形状,表面反照率,云散射,臭氧吸收以及气溶胶的散射和吸收。矿物粉尘吸收的辐射可使季节性平均仪器灵敏度降低50%。用GEOS-Chem模拟并用于AMF计算的平均SO2形状因子与机载现场测量(INTEX-A和INTEX-B)高度一致;差异将对检索到的SO2列产生10%的影响。取回的垂直柱通过同步的机载原位测量(INTEX-A,INTEX-B和在华东地区的一次运动)进行了验证。在受污染的地区(例如东亚和美国东部),年平均AMF误差估计为35-70%,在晴朗的海洋区域中不到10%。总体SO2误差评估为受污染地区的年平均水平为45-80%。 2006年从SCIAMACHY和OMI检索到的季节性平均SO2列与从GEOS-Chem检索到的季节性SO2列在空间上显着相关,尤其是在美国(SCIAMACHY和OMI的r = 0.85,0.82)。敏感性研究证实了SCIAMACHY和OMI对人为排放的SO2的敏感性。

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