Journal of Atmospheric and Environmental Optics ›› 2011, Vol. 6 ›› Issue (3): 179-184.

• 论文 • Previous Articles     Next Articles

Effect of Aerosol Vertical Distribution on Reflectance of Top of Atmosphere 

Zhou Kai-bing1,2,Yu Dong-sheng1,2,Xu Qing-shan1   

  1. (1 Key Laboratory of Atmospheric Composition and Optical Radiation, Center for Atmospheric Optics, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei 230031, China; 
    2 Graduate University of Chinese Academy of Sciences, Beijing 100039, China)
  • Received:2010-07-30 Revised:2010-08-31 Online:2011-05-28 Published:2011-05-23

Abstract:

In ocean-atmosphere system, errors may be resulted in retrieval of the water-leaving reflectance without regard to aerosol vertical distribution, so that, it affects the precision of ocean-color remote sensing. The effect of aerosol vertical distribution on the top of the atmosphere (TOA) reflectance was simulated by radiative transfer model. The result indicates that the error of the TOA reflectance (R) achieves 10%, especially 30%, while aerosol vertical distribution isn’t appropriate. The relative error (ΔR) increases with increasing aerosol optical thickness and aerosol absorption. The effect of relative azimuth angle on ΔR increases with increasing aerosol absorption. For strongly absorbing aerosols, R increases with decreasing the height of distribution.

Key words: aerosol, vertical distribution, top of the atmosphere, reflectance, absorption

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