Classification and change detection using Landsat TM data: When and how to correct atmospheric effects?

The electromagnetic radiation (EMR) signals collected by statellites in the solar spectrum are modified by scattering and absorption by gases and aerosols while traveling through the atmosphere from the Earth's surface to the sensor. When and how to correct the atmospheric effects depend un the remote sensing and atmospheric data available, the information desired and the analytical methods used to extract the information In many applications involving classification and change detection, atmospheric correction is unnecessary as long as the training data and the data to be classified nl-e in the same relative scale. In other circumstances, corrections al-e mandatory to put multitemporal data on the same radio-metric scale in order to monitor terrestrial surfaces over time. A multitemporal dataset consisting of seven Land-sat 5 Thematic Mapper (TM) images from 1988 to 1996 of the Pearl River Delta, Guangdong Province, China was used to compare sewn absolute and one relative atmospheric correction algorithms with uncorrected raw data. Based on classification and change detection results all corrections improved the data analysis. The best overall results are achieved using a new method which adds the effect of Rayleigh scattering to conventional dark object subtraction. Though this method may not lead to accurate surface reflectance, it best minimizes the difference in reflectances within a land cover class through time as measured with the Jeffries-Matusita distance. Contrary to expectations, the more complicated algorithms do not necessarily lend to improved performance of classification and change detection. Simple dark object subtraction, with or without the Rayleigh atmosphere correction, or relative atmospheric correction are recommended for classification, and change detection applications. (C) Elsevier Science Inc., 2001. All Rights Reserved.