Wave turbulence: Difference between revisions

Wave turbulence is a set of waves deviated far from thermal equilibrium. Such state is accompanied by dissipation. It is either decaying turbulence or requires external source of energy to sustain it. Examples are waves on a fluid surface excited by winds or ships, waves in plasma excited by electromagnetic waves etc. External sources by some resonant mechanism usually excite waves with frequencies and wavelengths in some narrow interval. For example, shaking container with the frequency ω excites surface waves with the frequency ω/2 (parametric resonance discovered by Faraday).

When wave amplitudes are small (which usually means that the wave is far from breaking), only those waves exist that are directly excited by an external source. When, however, wave amplitudes are not very small small (for surface waves when the fluid surface is inclined by more than few degrees) wave with different frequencies start to interact. That leads to an excitation of waves with frequencies and wavelengths in wide intervals, not necessarily in resonance with an external source. It can be observed in the experiments with a high amplitude of shaking that initially the waves appear which are in resonance, then both longer and shorter waves appear as a result of wave interaction. The appearance of shorter waves is referred to as a direct cascade while longer waves are part of an inverse cascade of wave turbulence.

Pedlosky, J (1987). Geophysical fluid dynamics. Springer.

Zakharov, V.E. (1992). Kolmogorov Spectra of Turbulence. Berlin: Springer-Verlag. {{cite book}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)