An Etymological Dictionary of Astronomy and Astrophysics

The temperature gradient defining the → radiative equilibrium
condition in a region. It is expressed as: dT/dr = (1 - 1/ γ)((T / P)(dP / dr), where T and P are temperature and pressure, dT / dr and dP / dr temperature and pressure gradients respectively, and γ = C_P / C_V.
For radiative equilibrium to be stable against → convection, the actual temperature gradient must be less than the adiabatic temperature gradient, i.e. |dT /dr|_rad < |dT /dr|_ad. See also → Schwarzschild’s criterion.

See also: → adiabatic; → temperature; → gradient.