Interaction of vorticity, rate-of-strain, and scalar gradient in stratified homogeneous sheared turbulence

DOI10.1063/1.870369zbMath1149.76359OpenAlexW2071229510MaRDI QIDQ3544158

K. K. Nomura, Peter J. Diamessis

Publication date: 5 December 2008

Published in: Physics of Fluids (Search for Journal in Brave)

Full work available at URL: https://semanticscholar.org/paper/5f9a0436b4bb66b984ad87895e414216c2ea22f8

Mathematics Subject Classification ID

Fluid mechanics (76-XX)

Related Items (16)

Effect of the shear parameter on velocity-gradient statistics in homogeneous turbulent shear flow ⋮ Flow topology in compressible turbulent boundary layer ⋮ The effect of stable stratification on turbulence anisotropy in uniformly sheared flow ⋮ Direct particle–fluid simulation of Kolmogorov-length-scale size particles in decaying isotropic turbulence ⋮ The scalar gradient alignment statistics of flame kernels and its modelling implications for turbulent premixed combustion ⋮ Study of the anisotropy of a passive scalar field at the level of dissipation ⋮ On the role of vorticity in the microstructure of a passive scalar field ⋮ Turbulence and fluid-front area production in binary-species, supercritical, transitional mixing layers ⋮ Anisotropy of a thermal field at dissipative scales in the case of small-scale injection ⋮ Geometrical properties of the resolved-scale velocity and temperature fields predicted using large-eddy simulation ⋮ The internal gravity wave field emitted by a stably stratified turbulent wake ⋮ Mixing in a stably stratified medium by horizontal shear near vertical walls ⋮ Interaction of turbulence and scalar fields in premixed flames ⋮ Large eddy simulation of turbulent statistical and transport properties in stably stratified flows ⋮ Similarity scaling and vorticity structure in high-Reynolds-number stably stratified turbulent wakes ⋮ Turbulence topologies predicted using large eddy simulations

Cites Work

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• Diffusion in stably stratified turbulence
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• Model dynamics and vertical collapse in decaying strongly stratified flows

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