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WKB theory for rapid distortion of inhomogeneous turbulence

dc.contributor.authorNazarenko, S.
dc.contributor.authorKevlahan, N.K.-R.
dc.contributor.authorDubrulle, B.
dc.date.accessioned2015-03-18T21:02:25Z
dc.date.available2015-03-18T21:02:25Z
dc.date.issued1999
dc.description.abstractA WKB method is used to extend RDT (rapid distortion theory) to initially inhomoge- neous turbulence and unsteady mean flows. The WKB equations describe turbulence wavepackets which are transported by the mean velocity and have wavenumbers which evolve due to the mean strain. The turbulence also modifies the mean flow and generates large-scale vorticity via the averaged Reynolds stress tensor. The theory is applied to Taylor’s four-roller flow in order to explain the experimentally observed reduction in the mean strain. The strain reduction occurs due to the formation of a large-scale vortex quadrupole structure from the turbulent spot confined by the four rollers. Both turbulence inhomogeneity and three-dimensionality are shown to be important for this effect. If the initially isotropic turbulence is either homogeneous in space or two-dimensional, it has no effect on the large-scale strain. Furthermore, the turbulent kinetic energy is conserved in the two-dimensional case, which has impor- tant consequences for the theory of two-dimensional turbulence. The analytical and numerical results presented here are in good qualitative agreement with experiment.en_US
dc.identifier.citationNazarenko, S., Kevlahan, N. K.-R. & Dubrulle, B. 1999 WKB theory for rapid distortion of inhomogeneous turbulence, J. Fluid Mech. 390, 325-348.en_US
dc.identifier.otherDOI:10.1017/S0022112099005340
dc.identifier.urihttp://hdl.handle.net/11375/16843
dc.language.isoenen_US
dc.publisherCambridge University Pressen_US
dc.relation.ispartofseriesJournal of Fluid Mechanics;
dc.subjectWKB theoryen_US
dc.subjectrapid distortion theoryen_US
dc.subjectturbulence theoryen_US
dc.titleWKB theory for rapid distortion of inhomogeneous turbulenceen_US
dc.typeArticleen_US

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