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integration variable, p a is the perturbation pressure, w a is the vertical velocity, and the integral is evaluated at z = − H ML = −40m. The favorable comparisons between the slab model and ROMS simulations shown in Figs. 11 and 12 suggest that the slab model is capable of representing the boundary layer dynamics of near-inertial motions even when the damping is associated with a substantially inviscid downward wave radiation process. In fact, the spatiotemporal maps of downward wave energy
integration variable, p a is the perturbation pressure, w a is the vertical velocity, and the integral is evaluated at z = − H ML = −40m. The favorable comparisons between the slab model and ROMS simulations shown in Figs. 11 and 12 suggest that the slab model is capable of representing the boundary layer dynamics of near-inertial motions even when the damping is associated with a substantially inviscid downward wave radiation process. In fact, the spatiotemporal maps of downward wave energy
