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Simulations of Aerosol Optical Properties to Top of Atmospheric Reflected Sunlight in the Near Infrared CO_2 Weak Absorption Band 被引量:6

Simulations of Aerosol Optical Properties to Top of Atmospheric Reflected Sunlight in the Near Infrared CO_2 Weak Absorption Band
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摘要 Over the Asian continent,high aerosol loading is critical to ensure the high accuracy of CO_2 retrieval in the near infrared absorption band.Simulations were performed to explore the effect of light path modification by aerosol son the atmospheric CO_2 near infrared band(6140-6270 cm^(-1)).The Vector LInearized Discrete Ordinate Radiative Transfer(VLIDORT) model and the Line-By-Line Radiative Transfer Model(LBLRTM) were used for forward calculations.The U.S.standard atmosphere was used for atmospheric profiles.The results indicate that the aerosols caused similar effects to increases in CO_2 in the planetary boundary layer and became more significant with aerosol layer rising while aerosol optical depth was 0.1.This effect will cause an over estimation of the CO_2 mixing ratio in the retrieval process and an under estimation in the aerosol layer.The results also indicate that the effect of urban and industrial aerosols is smaller than that of non-absorbing and dust aerosols because of the nearly constant absorption properties in the near infrared band. Over the Asian continent, high aerosol loading is critical to ensure the high accuracy of CO2 retrieval in the near infrared absorption band. Simulations were per- formed to explore the effect of light path modification by aerosol son the atmospheric CO2 near infrared band (6140-6270 cm-1). The Vector LInearized Discrete Ordi- nate Radiative Transfer (VLIDORT) model and the Line-By-Line Radiative Transfer Model (LBLRTM) were used for forward calculations. The U.S. standard atmos- phere was used for atmospheric profiles. The results indi- cate that the aerosols caused similar effects to increases in CO2 in the planetary boundary layer and became more significant with aerosol layer rising while aerosol optical depth was 0.1. This effect will cause an over estimation of the CO2 mixing ratio in the retrieval process and an under estimation in the aerosol layer. The results also indicate that the effect of urban and industrial aerosols is smaller than that of non-absorbing and dust aerosols because of the nearly constant absorption properties in the near in- frared band.
出处 《Atmospheric and Oceanic Science Letters》 CSCD 2013年第1期60-64,共5页 大气和海洋科学快报(英文版)
基金 funded by the Strategic Priority Research Program-Climate Change:Carbon Budget and Relevant Issues (Grant No. XDA05040200) the National High Techonology Research and Development Program of China (863 Program,Grant No. 2011AA12A104)
关键词 气溶胶光学厚度 近红外波段 标准大气 吸收带 CO2 光学特性 模拟 太阳光 satellite remote sensing, CO2, near infrared, aerosol
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