Also known as: UV aerosol index, aerosol absorbing index, or aerosol absorbing indicator.
The aerosol index is an index that indicates the presence of uv-absorbing aerosols such as dust and soot.
UV 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 & OMI, AI is defined as
AI = 100 * [ log10 (I360/I331)measured - log10 (I360/I331)calculated]
Positive values of the aerosol index generally represent absorbing aerosols (dust and smoke) while small or negative values represent non-absorbing 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 a similar index called the absorbing aerosols indicator (AAI). Following TOMS AI definition GOME AI 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.
UV Aerosol Index Data Pathfinder