Empirical studies report several plausible correlations between transf
orms of spectral reflectance, called vegetation indexes, and parameter
s descriptive of vegetation leaf area, biomass and physiological funct
ioning. However, most indexes can be generalized to show a derivative
of surface reflectance with respect to wavelength. This derivative is
a function of the optical properties of leaves and soil particles. In
the case of optically dense vegetation, the spectral derivative, and t
hus the indexes, can be rigorously shown to be indicative of the abund
ance and activity of the absorbers in the leaves. Therefore, the widel
y used broad-band red/near-infrared vegetation indexes are a measure o
f chlorophyll abundance and energy absorption.