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Numerical study of rotating turbulence with external forcing
Author(s) -
P. K. Yeung,
Ye Zhou
Publication year - 1998
Publication title -
physics of fluids
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.188
H-Index - 180
eISSN - 1089-7666
pISSN - 1070-6631
DOI - 10.1063/1.869810
Subject(s) - physics , turbulence , isotropy , reynolds stress , classical mechanics , wavenumber , anisotropy , rotation (mathematics) , mechanics , tensor (intrinsic definition) , scaling , reynolds number , forcing (mathematics) , statistical physics , inertial wave , computational physics , wave propagation , optics , geometry , mechanical wave , mathematics , atmospheric sciences , longitudinal wave
Direct numerical simulations at 2563 resolution have been carried out to study the response of isotropic turbulence to the concurrent effects of solid-body rotation and stochastic, isotropic forcing at the large scales. Because spectral transfer to the smaller scales is weakened by rotation, energy input from forcing gradually builds up at the large scales, causing the overall kinetic energy to increase. At intermediate wave numbers the energy spectrum undergoes a transition from a limited k−5/3 inertial range to k−2 scaling recently predicted in the literature. Although the Reynolds stress tensor remains approximately isotropic and three-component, evidence for anisotropy and quasi-two-dimensionality in length scales and spectra in different velocity components and directions is strong. The small scales are found to deviate from local isotropy, primarily as a result of anisotropic transfer from the large scales. To understand the spectral dynamics of this flow, we study the detailed behavior of nonlinear...

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