For a thin disk in the harmonic vertical gravitational potential , hydrostatic equilibrium and with height-independent isothermal sound speed give the displayed Gaussian density. For perturbations with adiabatic index , the Brunt–Väisälä frequency is . An isothermal background can therefore support buoyancy for adiabatic perturbations; isothermal perturbations instead have and zero buoyancy frequency.
A locally isothermal disk in vertically harmonic external gravity has hydrostatic equilibrium , hence with . Because is independent of height, integrating gives the displayed pressure. The harmonic-gravity approximation has the accuracy of the thin disk expansion.
In an inviscid locally isothermal Keplerian disk, a radial normal mode of wavenumber has pressure variable proportional to a Probabilists' Hermite polynomial in . Gaussian-weighted finite energy excludes the exponentially growing vertical branch. Polynomial termination gives and the local dispersion relation , where . At singular values introduced by eliminating velocity components, the original equations must also be checked. The propagating branch is an inertial-acoustic wave; has vertically uniform vertical velocity and odd pressure perturbation, permitting bending disturbances.
For the , Hermite vertical mode of an isothermal disk, the local dispersion relation is . Its low inertial-frame frequency branches satisfy . These waves transport a changing tilt of successive annuli, or a warp, with group velocity . The vertical velocity is approximately independent of height. A rigid tilt is the zero-wavenumber, zero-pattern-frequency limit; the gas still executes vertical orbital motion at frequency in its rotating frame.
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