For a circular orbit of cylindrical radius in an axisymmetric gravitational potential,
A small vertical displacement satisfies
so the vertical epicyclic frequency is
For a spherically symmetric potential , where ,
Hence . Geometrically, a slightly tilted circular orbit remains a circular orbit in a different plane, and its height completes one oscillation per revolution.
Vertical hydrostatic equilibrium gives
Define vertically integrated pressure and the density-weighted disk scale height by
Multiply the hydrostatic equation by and integrate. Since at both boundaries, integration by parts gives
Therefore
Introduce the dimensionless variables
Using , vertical hydrostatic equilibrium becomes the parameter-free equation
with normalizations and . For an isothermal atmosphere, , and these conventions give the Gaussian distribution
Gas in hydrostatic balance has zero vertical velocity. A dust grain subject to linear drag with aerodynamic stopping time therefore obeys
This is a damped harmonic oscillator. For , the motion is underdamped, with angular frequency
and envelope . Critical damping occurs at . For , the motion is overdamped. In the strong-drag limit , a rapid transient on timescale leaves slow dust settling in an astrophysical disk at rate ; in the weak-drag limit the grain makes many damped vertical oscillations.
Let label a fluid element and use the homologous vertical motion of an astrophysical disk
Because and , this ansatz satisfies mass conservation. The pressure equation for an adiabatic process gives
hence
The vertical acceleration is . Using the dimensionless hydrostatic profiles from part c, the pressure force is , and the vertical momentum equation reduces to
where is constant.
At the equilibrium thickness ,
Set and retain terms linear in . The linearization is
Thus the vertical breathing mode of an astrophysical disk has angular frequency

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