turbulentses

Turbulentses is a term used in some theoretical discussions to describe the ensemble of chaotic, multiscale fluctuations that characterize turbulent flows. It is not a standard term in mainstream turbulence research, but appears in speculative or conceptual writings as a way to denote the collective behavior of eddies across scales.

In these discussions, turbulentses is defined as the non-equilibrium state of a fluid where energy cascades from large to small scales through a hierarchy of interacting vortical structures, producing intermittent bursts and non-Gaussian statistics.

Key features include self-similarity or multifractality across a range of scales, intermittent energy dissipation, anisotropy at larger scales, and a strong dependence on Reynolds number.

Contexts where turbulentses is sometimes invoked include atmospheric boundary layer flows, ocean currents, laboratory plasma turbulence, combustion environments, and other complex fluids.

Measurement and modeling rely on velocity structure functions and spectral analyses, with the Kolmogorov -5/3 slope often cited alongside intermittency corrections via multifractal formalisms. Numerical simulations such as direct numerical simulation (DNS) and large-eddy simulation (LES), along with experimental techniques like particle image velocimetry (PIV), are used to study the proposed phenomena.

Relation to established concepts: turbulentses is closely related to turbulence and energy cascades but emphasizes collective, scale-spanning phenomena rather than single-scale descriptions.

See also: turbulence, chaotic dynamics, fractals, energy cascade.