2005/01/01 by В. Е. Захаров, V. E. Zakharov, A. O. Korotkevich +2 · 96 citations
Earth and Planetary Sciences · Mathematics · Physics and Astronomy · #Classical mechanics #Computer simulation #Differential Equations and Numerical Methods #K-epsilon turbulence model #K-omega turbulence model #Kinetic energy #Mechanics #Mesoscopic physics #Nonlinear Waves and Solitons #Ocean Waves and Remote Sensing #Physics #Quantum mechanics #Statistical physics #Turbulence #Turbulence kinetic energy #Wave turbulence #nlin.CD #physics.comp-ph #physics.flu-dyn
paper · pdf · doi:10.1134/1.2150867
published in Journal of Experimental and Theoretical Physics Letters 82(8), 487 (Pleiades Publishing) · 5 pages, 11 figures
openalex publication_date 2005/01/01 · arxiv created 2005/11/16 · arxiv updated 2022/06/03 · openalex created_date 2025/10/10 · openalex updated_date 2026/08/05
We report results of sumulation of wave turbulence. Both inverse and direct cascades are observed. The definition of "mesoscopic turbulence" is given. This is a regime when the number of modes in a system involved in turbulence is high enough to qualitatively simulate most of the processes but significantly smaller then the threshold which gives us quantitative agreement with the statistical description, such as kinetic equation. Such a regime takes place in numerical simulation, in essentially finite systems, etc.