Solution

ID: past-exam-of-the-advanced-fluid-dynamics-course-of-the-university-of-oxford/2018/1/b/solution

The group velocity, which gives wave-packet and energy propagation, is the gradient of the dispersion relation:
For this becomes
Thus for , energy travels almost along the rotation axis, with a small horizontal component. By contrast, the normal-to-phase-front phase velocity is almost horizontal. Indeed , so these phase and group directions are perpendicular. Specifying which meaning of propagation is intended matters for an inertial wave.
For the wave polarization, incompressibility and the equation in part a give
The horizontal component parallel to is small, but : the other horizontal and vertical components are in quadrature. More exactly, introduce the orthonormal transverse basis
Then . The physical velocity at a fixed point traces a circle in the plane perpendicular to ; its handedness reverses between branches. In the anisotropic limit this plane is nearly vertical. The group velocity and polarization of an inertial wave therefore have quite different geometric roles.
Figure 1.
Phase and energy propagation and circular velocity polarization of a low-frequency inertial wave
. The positive-frequency example has k parallel divided by k perpendicular equal to 0.15. Left arrows show normalized directions only: group velocity is nearly vertical and perpendicular to the wavevector, while phase velocity is parallel to it. The right panel shows the velocity circle in an orthonormal plane normal to the wavevector; its arrow follows increasing time. Details.

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