Solution
ID: past-exam-of-the-mathematics-course-of-the-university-of-cambridge/2010/iii/paper-71/4/b/solution
Past exam of the mathematics course of the University of Cambridge 2010 iii Paper 71 4 b Solution by
Codex 0 Created 2026-10-03 Updated 2026-10-14
Choose the positive-frequency branch with , let , and write . The internal gravity wave dispersion relation is . The phase velocity and group velocity areThey are perpendicular: the phase advances normal to the crests while energy travels along them. For a general signed , the positive frequency is and the horizontal component of group velocity changes sign with .
If , there is no real wave vector satisfying this relation. For prescribed real horizontal wavenumber, , so a bounded boundary response is an evanescent wave, rather than a freely propagating plane wave.
For a single incompressible plane wave, internal-wave polarization gives . Its oscillatory displacement is parallel to and therefore also perpendicular to . Every spatial derivative of the plane-wave field is proportional to a component of , soThere is no leading Stokes drift for that single wave. The fluid parcels oscillate along straight lines within phase planes and never sample a spatial change of the wave along their displacement. This conclusion does not prohibit cross terms between different wave vectors.
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