The 8- to 14-m region of spectral radiant exitance is of particular interest since it not only includes an atmospheric window but also contains the peak energy emissions for most surface features on earth. That is, the ambient temperature of earth surface features is normally about 300 K, at which temperature the peak emissions will occur at approximately 9.7 m. For these reasons, most thermal sensing is performed in the 8- to 14-m region of the spectrum.