Write the density and pressure as and , respectively. The background satisfies hydrostatic balance, , and . Linearizing the Euler equations for an inviscid fluid, incompressibility and advection of density givesDifferentiate the horizontal equation in and use incompressibility to obtain . Differentiate the vertical equation in time and twice in :Dividing by gives the equation for internal waves in an exponentially stratified incompressible fluid,The first-derivative term retains the variation of inertial density with height; no Boussinesq approximation has been made.
For , direct differentiation givesThus the transformed partial differential equation and its impermeable-wall boundary conditions areThe positive exponential factor does not change where the vertical velocity vanishes.
Substitute into the transformed equation. It yieldsThe nonzero eigenfunctions of this Dirichlet boundary value problem are , . Hence, with and ,The physical vertical velocity includes the factor . The zero horizontal wavenumber is the zero-frequency limiting case, not a propagating oscillation.
Choose the rightgoing signed dispersion relation . The horizontal phase velocity and group velocity areThe leftgoing branch has their negatives. For a convention using positive frequency at both signs of , multiply each displayed speed by . For every nonzero , on the rightgoing branch; the horizontal group-speed bound for a confined internal wave is , approached as .
Use the Fourier transform convention , with inverse factor . The initial profile occupies only the vertical mode . Its transform isThe transformed evolution is a harmonic oscillator for each , withTherefore inversion givesUsing the nonnegative even frequency instead gives the same cosine. At , with , recovering the specified initial profile and its zero time derivative.
Write the cosine in i as two complex exponentials. On a ray , the oscillatory phases are . The stationary phase method requires . By ii, the largest absolute horizontal group velocity for the occupied mode isInside this region there are stationary wavenumbers supporting appreciable wave packet contributions. Outside it no stationary wavenumber exists; oscillatory cancellation suppresses the large-time response. This explains "mainly confined": the initial Lorentzian profile already has nonzero algebraic tails, so the displayed region is not the exact support of the solution. Near its boundary the stationary points meet and the usual nondegenerate stationary-phase formula needs a transition approximation.
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