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Gregory P. Asner, David E. Knapp, Amanda N. Cooper, Mercedes M. C. Bustamante, and Lydia P. Olander

program is integrated into the CLAS processing stream and uses average monthly aerosol optical thickness (AOT) and water vapor (WV) values from the NASA MODIS sensor. Time stamping of MODIS AOT and WV with Landsat data is done on an automated basis ( Figure 3 ). A series of masks are designed to exclude clouds, water bodies, cloud shadows, and nonimage areas from the analysis. These masks are derived directly from the raw and calibrated Landsat imagery as well as from the AutoMCU submodel output of

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