It is an index that detects the presence of uv-absorbing aerosols such as dust and soot.
TOMS Aerosol index (AI) is based on a spectral contrast method in a UV region where the ozone
absorption is very small. It is the difference between the observations and model
calculations of absorbing and non absorbing spectral radiance ratios. For TOMS, AI is
defined as
AI = 100 [ log10 (I360/I331)measured
- log10 (I360/I331)calculated]
Positive values of Aerosol Index generally represent
absorbing aerosols (dust and smoke) while small or negative values represent
nonabsorbing aerosols and clouds. The Index can be interpreted in terms of
optical depth if the index of refraction, particle size distribution, and the
height of the aerosol layer are known from other measurements.
GOME (ERS-2) defines similar index called Absorbing Aerosols Indicator
(AAI). Following TOMS AI definition GOME AAI also uses two wavelength intervals
around 340 nm and 380 nm.
However, POLDER on ADEOS-1 & 2 define Aerosol Index (for small size
particles) as the product of the retrieved aerosol optical thickness and
Angstrom exponent.