1.4.4 Static case

Further assumption:

$\begin{displaymath} v_{x} = v_{y} = v_{z} = 0 \end{displaymath}$

(37)

Result:

No mass loss

Hydrostatic pressure stratification:

$\begin{displaymath} \frac{\partial }{\partial z} \left( \langle P\rangle + \la... ...{\mathrm{rad},z} \rangle \right) = - \langle \rho \rangle g \end{displaymath}$

(38)

Stratification in radiative equilibrium:

$\begin{displaymath} \langle F_{\mathrm{rad},z} \rangle = \mathrm{const} = F_{*} \end{displaymath}$

(39)