The Minnaert function is a photometric function used to interpret astronomical observations and remote sensing data for the Earth. It was named after the astronomer Marcel Minnaert. This function expresses the radiance factor (RADF) as a function the phase angle ( α {\displaystyle \alpha } ), the photometric latitude ( φ {\displaystyle \varphi } ) and the photometric longitude ( λ {\displaystyle \lambda } ).
where A M {\displaystyle A_{M}} is the Minnaert albedo, k {\displaystyle k} is an empirical parameter, I {\displaystyle I} is the scattered radiance in the direction ( α , φ , λ ) {\displaystyle (\alpha ,\varphi ,\lambda )} , π F {\displaystyle \pi F} is the incident radiance, and
The phase angle is the angle between the light source and the observer with the object as the center.
The assumptions made are:
Minnaert's contribution is the introduction of the parameter k {\displaystyle k} , having a value between 0 and 1, originally for a better interpretation of observations of the Moon. In remote sensing the use of this function is referred to as Minnaert topographic correction, a necessity when interpreting images of rough terrain.