Propagating and evanescent internal waves in a deep ocean model

Abstract

AbstractWe present experimental and computational studies of the propagation of internal waves in a stratified fluid with an exponential density profile that models the deep ocean. The buoyancy frequency profile $N(z)$ (proportional to the square root of the density gradient) varies smoothly by more than an order of magnitude over the fluid depth, as is common in the deep ocean. The non-uniform stratification is characterized by a turning depth ${z}_{c} $, where $N({z}_{c} )$ is equal to the wave frequency $\omega $ and $N(z\lt {z}_{c} )\lt \omega $. Internal waves reflect from the turning depth and become evanescent below the turning depth. The energy flux below the turning depth is shown to decay exponentially with a decay constant given by ${k}_{c} $, which is the horizontal wavenumber at the turning depth. The viscous decay of the vertical velocity amplitude of the incoming and reflected waves above the turning depth agree within a few per cent with a previously untested theory for a fluid of arbitrary stratification (Kistovich and Chashechkin, J. Appl. Mech. Tech. Phys., vol. 39, 1998, pp. 729–737).