Coupling of Waves to Sea Surface Currents Via Horizontal Density Gradients

Abstract

The mathematical models and numerical simulations reported here are motivated by satellite observations of horizontal gradients of sea surface temperature and salinity that are closely coordinated with the slowly varying envelope of the rapidly oscillating waves. This coordination of gradients of fluid material properties with wave envelopes tends to occur when strong horizontal buoyancy gradients are present. The nonlinear models of this coordinated movement presented here may provide future opportunities for the optimal design of satellite imagery that could simultaneously capture the dynamics of both waves and currents directly.The model derived here appears in two levels of approximation: first for rapidly oscillating waves, and then for their slowly varying envelope (SVE) approximation obtained by using the WKB approach. The WKB wave-current-buoyancy interaction model derived here for a free surface with significant horizontal buoyancy gradients indicates that the mechanism for the emergence of these correlations is the ponderomotive force of the slowly varying envelope of rapidly oscillating waves acting on the surface currents via the horizontal buoyancy gradient. In this model, the buoyancy gradient appears explicitly in the WKB wave momentum, which in turn generates density-weighted potential vorticity whenever the buoyancy gradient is not aligned with the wave-envelope gradient.

On the interactions between mean flows and inertial gravity waves

“…By writing the Hamiltonian in terms of the mean flow momentum, m, rather than the total momentum, M, we recover the tangled version of the Lie-Poisson Hamiltonian form of the equations. Above, as in [12], we have presented wave-current interaction in its untangled form. In a previous work [11], the authors presented both the tangled and untangled forms, and an analogous calculation is also possible for this model of WMFI.…”