Optical depth gives a measure of how opaque a medium is to radiation passing through it. It is measured along the
vertical optical path dz and, in the planetary science convention, is measured downwards from the top of the
atmosphere, so that
Integrating for normal incidence gives
where N is the column density.
Extinction Coefficient, Law of Atmospheres, Opacity, Optical Path, Radiative Transfer, Radiative Transfer Equation, Scale Height