A streamline coordinate system for distorted two-dimensional shear flows
- 1 May 1983
- journal article
- research article
- Published by Cambridge University Press (CUP) in Journal of Fluid Mechanics
- Vol. 130 (-1) , 241-258
- https://doi.org/10.1017/s002211208300107x
Abstract
A function ϕ is derived which is constant along the orthogonal trajectories of streamlines in two-dimensional flow. In irrotational flows, ϕ reduces to the velocity potential. The pair of functions ϕ and ψ, where ψ is the stream function, are used to define a coordinate system in rotational fluid flows. Tensor methods are used to transform the equations of motion of a turbulent fluid and the equations for second moments of turbulent fluctuations to this coordinate system. Explicit extra terms appear in the transformed equations embodying the effects of streamline curvature and mean flow acceleration. These extra terms are characterized by two lengthscales which arise naturally from the transformation: the local radius of curvature of the streamline and the ‘e-folding’ distance of the mean streamwise velocity.Keywords
This publication has 8 references indexed in Scilit:
- The interaction between an internal gravity wave and the planetary boundary layer. Part II: Effect of the wave on the turbulence structureQuarterly Journal of the Royal Meteorological Society, 1981
- A wind-tunnel study of turbulent flow close to regularly arrayed rough surfacesBoundary-Layer Meteorology, 1980
- The turbulence structure of a highly curved mixing layerJournal of Fluid Mechanics, 1976
- The analogy between streamline curvature and buoyancy in turbulent shear flowJournal of Fluid Mechanics, 1969
- Viscoelastic properties of fine-grained incompressible turbulenceJournal of Fluid Mechanics, 1968
- Curved Turbulent Mixing LayerPhysics of Fluids, 1965
- DriftJournal of Fluid Mechanics, 1956
- The physical components of vectors and tensorsZAMM - Journal of Applied Mathematics and Mechanics / Zeitschrift für Angewandte Mathematik und Mechanik, 1953