On transport across a barotropic shear flow by breaking inertia-gravity waves
Résumé
We investigate the interaction of an inertia-gravity wave packet with a barotropic dynamical barrier, by means of three-dimensional direct numerical simulations of the Boussinesq equations in a rotating reference frame. A simple model is used for the barrier, namely a barotropic shear layer with a horizontal shear. We show that the increase of the intrinsic frequency Ω of the wave packet by Doppler shifting may result in the breaking of the wave packet, in the neighborhood of a trapping plane where Ω=N(N is the Brunt–Väisälä frequency of the fluid and is constant in the present study). The breaking process triggers a turbulent diffusive transport of mass and momentum across the barrier, with a turbulent Prandtl number of order 1.
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