Flow, Turbulence and Combustion 73: 277–305, 2004. © 2004 Kluwer Academic Publishers. Printed in the Netherlands. 277 Direct Numerical Simulation of a Turbulent Axisymmetric Jet with Buoyancy Induced Acceleration AMIT AGRAWAL 1 , B.J. BOERSMA 2 and AJAY K. PRASAD 3 1 Discipline of Mechanical Engineering, University of Newcastle, NSW 2308, Australia; E-mail: amit.agrawal@newcastle.edu.au 2 Laboratory of Aero and Hydrodynamics, Delft University of Technology, 2628 CA Delft, The Netherlands; E-mail: b.j.boersma@wbmt.tudelft.nl, 3 Department of Mechanical Engineering, University of Delaware, Newark, DE 19716, U.S.A.; E-mail: prasad@me.udel.edu Received 6 November 2002; accepted in revised form 20 January 2004 Abstract. Direct numerical simulations of an axisymmetric jet with off-source volumetric heat addition are presented in this paper. The system solved here involves a three-way coupling between velocity, concentration and temperature. The computations are performed on a spherical coordinate system, and application of a traction free boundary condition at the lateral edges allows physical entrainment into the computational domain. The Reynolds and Richardson numbers based on local scales employed in the simulations are 1000 and 12 respectively. A strong effect of heat addition on the jet is apparent. Heating causes acceleration of the jet, and an increased dilution due to an increase in entrainment. Further, the streamwise velocity profile is distorted, and the cross-stream velocity is inward for all radial locations for the heated jet. Interestingly, the maximum temperature is realized off-axis and a short distance upstream of the exit of the heat injection zone (HIZ). The temperature width is intermediate between the scalar and velocity widths in the HIZ. Normalized rms of the concentration and temperature increases in the HIZ, whereas that of streamwise, cross- stream and tangential velocities increases rapidly after decreasing. Both mass flux and entrainment are larger for the heated jet as compared to their unheated counterparts. The buoyancy flux increases monotonically in the HIZ, and subsequently remains constant. Key words: buoyancy flux, cumulus clouds, direct numerical simulation (DNS), entrainment, jets and plumes, mass flux, off-source volumetric heating. 1. Introduction An interesting and well known phenomenon is observed in cumulus clouds: as the heated column of air (plume) rises through the atmosphere and passes through the cloud base (the vertical location at which water vapor begins to condense to form droplets, thus rendering the cloud visible), its entrainment behavior changes drastically. Field observations of Colorado cumuli [19] clearly show that entrained air in a cumulus cloud originates either from the cloud base or from the cloud top, i.e., lateral entrainment of ambient air into the cloud virtually shuts down,