The greater shear associated with
the inertial frequency waves leads to enhanced dissipation in a thick layer above the topography.
Not exact matches
The other major source of internal
waves is the wind which produces internal
waves near the
inertial frequency.
Those
waves dominate the vertical velocity field in the mixed layer (vortex Rossby
waves) and below the first hundred meters (near
inertial waves) and they are responsible for the differences in the vertical transport properties under the various forcing fields as quantified by
frequency spectra, vertical velocity profiles and vertical dispersion of Lagrangian tracers.
If the wind field contains energy at the
inertial frequency or higher (daily and six - hourly cases), then Vortex Rossby
waves and near
inertial waves are excited as ageostrophic expression of the vigorous eddy field.