We calculate the net instantaneous power exchanged between two sets of modes in a generic system governed by a three-wave kinetic equation. In a first application to isotropic systems, we rederive the standard formula for the energy flux as a particular case for adjacent sets. We then exploit the new formalism to quantify nonlocal energy transfers in the example of surface capillary waves. These results establish a wave turbulence analog of the DIA formalism of Kraichnan (1959) for isotropic turbulence. A second application to nonisotropic wave systems expands the currently available set of tools to investigate magnitude and direction of the energy fluxes in these systems. We illustrate the use of the formalism by characterizing the energy ...
The energy flux in a finite-depth gravity-wave spectrum resulting from weak non-linear couplings bet...
We analyse the inter-scale transfer of energy for two types of plane Poiseuille flow: the P4U exact ...
Real turbulent flows are difficult to classify as either spatially homogeneous or isotropic. Nonethe...
Turbulence in a system of nonlinearly interacting waves is referred to as wave turbulence. It has be...
Turbulence is a ubiquitous state for many flows in nature and engineering. As the flow velocity is i...
It is theoretically established that energy transfer in nonhomogeneous turbulence occurs in two dist...
An up-to-date comprehensive text useful for graduate students and academic researchers in the field ...
Author Posting. © American Meteorological Society, 2022. This article is posted here by permission o...
We present an idealized representation of high frequency oceanic internal waves propagating in a bac...
In the early 1960s, it was established that the stochastic initial value problem for weakly coupled ...
International audienceAn important characteristic of geophysically turbulent flows is the transfer o...
The kinetic equation for non-linear wave-wave interactions for empirical wave energy spectra is di...
Theory is developed and utilized for the calculation of the separate transport of kinetic, gravity p...
In addition to their own convective breaking, the energetic baroclinic tides at a generation site st...
This paper investigates the effect of wave motion on the turbulence in close proximity to the surfac...
The energy flux in a finite-depth gravity-wave spectrum resulting from weak non-linear couplings bet...
We analyse the inter-scale transfer of energy for two types of plane Poiseuille flow: the P4U exact ...
Real turbulent flows are difficult to classify as either spatially homogeneous or isotropic. Nonethe...
Turbulence in a system of nonlinearly interacting waves is referred to as wave turbulence. It has be...
Turbulence is a ubiquitous state for many flows in nature and engineering. As the flow velocity is i...
It is theoretically established that energy transfer in nonhomogeneous turbulence occurs in two dist...
An up-to-date comprehensive text useful for graduate students and academic researchers in the field ...
Author Posting. © American Meteorological Society, 2022. This article is posted here by permission o...
We present an idealized representation of high frequency oceanic internal waves propagating in a bac...
In the early 1960s, it was established that the stochastic initial value problem for weakly coupled ...
International audienceAn important characteristic of geophysically turbulent flows is the transfer o...
The kinetic equation for non-linear wave-wave interactions for empirical wave energy spectra is di...
Theory is developed and utilized for the calculation of the separate transport of kinetic, gravity p...
In addition to their own convective breaking, the energetic baroclinic tides at a generation site st...
This paper investigates the effect of wave motion on the turbulence in close proximity to the surfac...
The energy flux in a finite-depth gravity-wave spectrum resulting from weak non-linear couplings bet...
We analyse the inter-scale transfer of energy for two types of plane Poiseuille flow: the P4U exact ...
Real turbulent flows are difficult to classify as either spatially homogeneous or isotropic. Nonethe...