Abstract
The influence of the lack of atmospheric correction of the optical images used to calculate land surface emissivity (LSE) was assessed. When thermal emissivity is determined by the vegetation cover method (VCM), information from the solar spectrum is required to calculate the vegetation cover fraction. The atmospheric correction was obtained in this study by using a combination of the dark dense vegetation (DDV) method and the Second Simulation of the Satellite Signal in the Solar Spectrum (6S) code. The methodology was applied to a Landsat Thematic Mapper (TM) image of Tomelloso, Spain. We determined that the emissivity between 10 and 12 µm only increases by 0.4% (which represents a systematic error of approximately +0.2 K) when atmospherically corrected reflectances are used in relation to non‐corrected Tomelloso scenes. Nevertheless, other test areas could yield larger differences.
Acknowledgements
We thank Drs Eva María Rubio and María del Mar Artiago of Castilla La Mancha University for the information provided on the Tomelloso image, and Dr Eric F. Vermote of Maryland University for his explanations concerning the atmospheric correction.