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Estimation of Surface Reflectance by Utilizing Single Visible Reflectance from COMS Meteorological Imager, Analysis of BAOD correction effect

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Yoon,  Jongmin
Atmospheric Chemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Citation

Kim, M., Kim, J., & Yoon, J. (2014). Estimation of Surface Reflectance by Utilizing Single Visible Reflectance from COMS Meteorological Imager, Analysis of BAOD correction effect. Korean Journal of Remote Sensing, 30(5), 627-639. doi:10.7780/kjrs.2014.30.5.8.


Cite as: https://hdl.handle.net/11858/00-001M-0000-0024-E388-7
Abstract
Accurate correction of surface effect from back scattered solar radiance is one of key issue to retrieve aerosol information from satellite measurements. In this study, two different methods are applied to retrieve surface reflectance by using single visible channel measurement from meteorological imager onboard COMS. The first one is minimum reflectance method, which composes the minimum value among previously measured reflectances at each pixel over a certain search window length. This method assumes that the darkest pixel corresponds to the aerosol-free condition, and deduces surface reflectance by correcting atmospheric scattering from the measured visible reflectance. The second method, named as the "atmospheric correction method" in this study, estimates the result by correcting aerosol and atmospheric scattering with ground-based observation of aerosol optical properties. The purpose of this study is to investigate the retrieval accuracy of the widelyused minimum reflectance method. Also, the retrieval error caused by the loading of background aerosol is mainly estimated. The comparison between surface reflectances retrieved from the two methods shows good agreement with the correlation coefficient of 0.87. However, the results from the minimum reflectance method are slightly overestimated than the values from the atmospheric correction method when surface reflectance is lower than 0.2. The average difference between the two results is 0.012 without the background aerosol correction. By considering the background aerosol effect, however, the difference is reduced to 0.010.