Self-regulation of deep-ocean internal wave continuum: Observations on related near-inertial shear and high-frequency vertical motions

Physics – Geophysics

Scientific paper

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Oceanography: Physical: Internal And Inertial Waves, Oceanography: Physical: Coriolis Effects, Oceanography: General: Time Series Experiments (1872, 3270, 4475), Nonlinear Geophysics: Self-Organization, Nonlinear Geophysics: Nonlinear Waves, Shock Waves, Solitons (0689, 2487, 3280, 3285, 4275, 6934, 7851, 7852)

Scientific paper

It is shown using detailed yearlong acoustic current observations between 850 and 1350 m that large-scale and small-scale waves in the ocean interior are coupled in a self-regulating fashion. Vertical current shear, a key to vertical mixing, is dominated near the local inertial frequency. Its value follows details of maximum buoyancy frequency `Nmax' in thin layers of different density. Its frequency however, is determined by the minimum Nmin in the near-homogeneous layers between the Nmax-layers. These weakly stratified layers are maintained by overturning of density surfaces due to high-frequency internal waves guided by the shear-layers. Rare vertical current observations show a spectral continuum between [Nmin, Nmax] of low-mode interfacial waves rather than wave-groups propagating through smooth large-scale stratification.

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