Energy transfer in resonant and near-resonant internal wave triads for weakly non-uniform stratifications. Part I: Unbounded domain

TL;DR

This paper develops a mathematical model to analyze energy transfer in internal wave triads within weakly non-uniform stratifications, considering effects like viscosity and rotation, and identifies key parameters influencing energy exchange.

Contribution

It introduces a generalized model for amplitude evolution in internal wave triads, accounting for non-uniform stratification and detuning effects, and defines new non-dimensional numbers to predict energy transfer.

Findings

Detuning significantly affects energy transfer in stratified media.

New non-dimensional numbers predict maximum energy transfer.

Small stratification changes can greatly influence wave interactions.

Abstract

In this paper, using multiple scale analysis we derive a generalized mathematical model for amplitude evolution, and for calculating the energy exchange in resonant and near-resonant global triads consisting of weakly nonlinear internal gravity wave packets in weakly non-uniform density stratifications in an unbounded domain in the presence of viscous and rotational effects. Such triad interactions are one of the mechanisms by which high wavenumber internal waves lead to ocean turbulence and mixing via parametric subharmonic instability. Non-uniform stratification introduces detuning - mismatch in the vertical wavenumber triad condition, which may strongly affect the energy transfer process. We investigate in detail how factors like wave-packets' width, group speeds, nonlinear coupling coefficients, detuning, and viscosity affect energy transfer in weakly varying stratification. We find limitations of the well-known 'pump-wave approximation' and derive a non-dimensional number, which can be evaluated from initial conditions, that can predict the maximum energy transferred from the primary wave during the later stages. Two additional non-dimensional numbers, based on various factors affecting energy transfer between near-resonant wave-packets have also been defined. Moreover, we identify the optimal background stratification in a medium of varying stratification for the primary wave to form a triad with no detuning so that the energy transfer is maximum. Finally, we show that even a small change in the background stratification can cause a significant difference in the energy transfer process between the wave-packets when they have the same order of magnitude of energy.