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      Energy-consistent entrainment relations for jets and plumes

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      Journal of Fluid Mechanics
      Cambridge University Press (CUP)

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          Abstract

          We discuss energetic restrictions on the entrainment coefficient ${\it\alpha}$ for axisymmetric jets and plumes. The resulting entrainment relation includes contributions from the mean flow, turbulence and pressure, fundamentally linking ${\it\alpha}$ to the production of turbulence kinetic energy, the plume Richardson number $\mathit{Ri}$ and the profile coefficients associated with the shape of the buoyancy and velocity profiles. This entrainment relation generalises the work by Kaminski et al. ( J. Fluid Mech., vol. 526, 2005, pp. 361–376) and Fox ( J. Geophys. Res., vol. 75, 1970, pp. 6818–6835). The energetic viewpoint provides a unified framework with which to analyse the classical entrainment models implied by the plume theories of Morton et al.( Proc. R. Soc. Lond.A, vol. 234, 1955, pp. 1–23) and Priestley & Ball ( Q. J. R. Meteorol. Soc., vol. 81, 1954, pp. 144–157). Data for pure jets and plumes in unstratified environments indicate that to first order the physics is captured by the Priestley and Ball entrainment model, implying that (1) the profile coefficient associated with the production of turbulence kinetic energy has approximately the same value for pure plumes and jets, (2) the value of ${\it\alpha}$ for a pure plume is roughly a factor of $5/3$ larger than for a jet and (3) the enhanced entrainment coefficient in plumes is primarily associated with the behaviour of the mean flow and not with buoyancy-enhanced turbulence. Theoretical suggestions are made on how entrainment can be systematically studied by creating constant- $\mathit{Ri}$ flows in a numerical simulation or laboratory experiment.

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          Most cited references33

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          Turbulent entrainment: the development of the entrainment assumption, and its application to geophysical flows

          J S Turner (1986)
          The entrainment assumption, relating the inflow velocity to the local mean velocity of a turbulent flow, has been used successfully to describe natural phenomena over a wide range of scales. Its first application was to plumes rising in stably stratified surroundings, and it has been extended to inclined plumes (gravity currents) and related problems by adding the effect of buoyancy forces, which inhibit mixing across a density interface. More recently, the influence of viscosity differences between a turbulent flow and its surroundings has been studied. This paper surveys the background theory and the laboratory experiments that have been used to understand and quantify each of these phenomena, and discusses their applications in the atmosphere, the ocean and various geological contexts.
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            Measurements of entrainment by axisymmetrical turbulent jets

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              Turbulent Jets and Plumes

              E. List (1982)
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                Author and article information

                Journal
                applab
                Journal of Fluid Mechanics
                J. Fluid Mech.
                Cambridge University Press (CUP)
                0022-1120
                1469-7645
                November 10 2015
                October 8 2015
                November 2015
                : 782
                : 333-355
                Article
                10.1017/jfm.2015.534
                7533468b-ee23-49c7-8c2f-0f6590cc91dd
                © 2015
                History

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