Abstract
A solution for a concentrated line front translating at speed U is given. It is shown that the frequency is near-inertial if U≫c1, where c1 is the long internal wave speed of the first baroclinic mode. Each more has a charactristic frequency ωn associated with it. The spectra contain a near-inertial primary peak, composed of the higher modes, whose blue shift increases with depth. They also contain secondary peaks at higher internal wave frequencies if U is only slightly larger than c1. The flow field is intermittent, and involves a continuous interchange of energy between the surface layer and the stratified interior. The dominant period of this intermittency is the beating period of the first mode with a purely inertial oscillation. Short periods of apparent subinertial motion are also generated. Several features of the solution are in agreement with observations.
