APPLYING BAND RATIOS TO HYPERSPECTRAL IMAGERY DATA
Band ratioing has a long history of successful application to multispectral data. Band ratios are used to suppress illumination differences attributable to surface albedo, look angle, and topographic effects. As pointed out by Vincent (1997), and Crippen (1988) proper data preparation is essential for the successful use of band ratios. There are two spectral components that must be accounted for when using band ratios: additive and multiplicative. The additive (sensor calibration and path radiance) component must be removed prior to performing a band ratio. The additive component to the signal can be most easily removed by performing a dark subtraction on each band. The multiplicative (radiance illumination and atmospheric absorption) component must be nearly equal for each band in the ratio. The best method for making the multiplicative component nearly equal for each band in the ratio is to choose contiguous, or nearly contiguous bands. Further quantitative support for the use of band ratios is given based on derivatives of spectra. Using derivatives constraints on the distance in wavelengths between bands used for ratios.
It is also important to remember that band ratios work best when applied to distinct absorption features such as the kaolinite (2135 2225 nm) doublet versus broad Fe absorption features located at wavelengths less than 1000 nm.
Band ratios are an excellent tool for performing preliminary evaluations of hyperspectral data. Examples are given for Copper Flat porphyry copper deposit and Cuprite, NV to demonstrate band ratios capabilities as a reconnaissance tool.