A new non-hydrostatic framework for the oceanic internal gravity wave spectrum formulated in horizontal wavenumber-vertical mode space that extends the Garrett-Munk model to arbitrary stratification and boundary conditions.
C., 1989: Scaling turbulent dissipation in the thermocline
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Toward a Universal Framework for the Internal Gravity Wave Spectrum
A new non-hydrostatic framework for the oceanic internal gravity wave spectrum formulated in horizontal wavenumber-vertical mode space that extends the Garrett-Munk model to arbitrary stratification and boundary conditions.