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Instabilities in variable-property flows and the continuous spectrum An aggressive ‘passive’ scalar. Harish Dixit and Rama Govindarajan With Anubhab Roy and Ganesh Subramanian Jawaharlal Nehru Centre for Advanced Scientific Research, Bangalore September 2008. Re=3000, unstratified.
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Instabilities in variable-property flows and the continuous spectrum An aggressive ‘passive’ scalar Harish Dixit and Rama Govindarajan With Anubhab Roy and Ganesh Subramanian Jawaharlal Nehru Centre for Advanced Scientific Research, Bangalore September 2008
Re=3000, unstratified Building block for inverse cascade
y 2 1 Light ρ(y) ρ Heavy `Perpendicular’ density stratification: baroclinic torque (+ centrifugal + other non-Boussinesq effects) Brandt and Nomura, JFM (2007): stratification upto Fr=2, Boussinesq Stratification aids merger at Re > 2000 At lower diffusivities, larger stratifications?
Large scale overturning: a separate story Why does the breakdown happen? Consider one vortex in a (sharp) density gradient In 2D, no gravity
Initial condition: Point vortex at a density jump Light point vortex Heavy
A single vortex and a density interface Inviscid Homogenised within the yellow patch, if Pe finite The locus seen is not a streamline!
Scaling Density is homogenised for e.g. Rhines and Young (1983) Flohr and Vassilicos (1997) (different from Moore & Saffman 1975) When Pe >>> 1, many density jumps between rh and rs Consider one such jump, assume circular
Non-Boussinesq: e.g. Turner, 1957, Sipp et al., Joly et al., JFM 2005 Point vortex, circular density jump Linearly unstable when heavy inside light, Rayleigh-Taylor Rotates at m times angular velocity of mean flow Non-Boussinesq, centrifugal Radial gravity Vortex sheet of strength
m = 2 Vortex sheet at rj In unstratified case: a continuous spectrum of `non-Kelvin’ modes
r Rankine vortex with density jumps at rjs spaced at r3 Kelvin (1880): neutral modes at r=a for a Rankine vortex
For one density jump For j jumps: 2j+2 boundary conditions ur and pressure continuous at jumps and rc Green’s function, integrating across jumps For non-Boussinesq case:
Multiple (7) jumps m = 5
Single jump Step vs smooth density change rj = 2 rc, =0.1
Single jump: radial gravity (blue), non-Boussinesq (red) m = 2, = 0.01
(circular jump: pressure balances, but) Lituus spiral Dominant effect, small a (non-dimensional) In the basic flow a KH instability at positive and negative jump growing faster than exponentially
Simulations: spectral, interfaces thin tanh, up to 15362 periodic b.c. Light Heavy Non-Boussinesq equations
Boussinesq, g=0, density is a passive scalar t=1.59 t=0 6.4 3.18
9.5 t=12.7
Vorticity time=0 time=12.7
1.6 Non-Boussinesq A=0.2 3.82
Viscous simulations: same instability A=0.12, t = 7.5Г/rc2 λ ~ 2.5ld (λstab ~ 4ld)
Re = 8000, Pe = 80000, rho1 = 0.9, rho2 = 1.1 (tanh interface), Circulation=0.8, thickness of the interface = 0.02, rc = 0.1, time = 2.5, N=1024 points Initial condition: Gaussian vortex at a tanh interface
Conclusions: Co-existing instabilities: `forward cascade’ unstable wins Beware of Boussinesq, even at small A What does this do to 2D turbulence?
Single jump: Boussinesq (blue), non-Boussinesq (red) m = 20, = 0.1
Variation of ur eigenfunction with the jump location: rc = 0.1, m = 2
Effect of large density differences m = 2, = 1
2D simulations of Harish: Boussinesq approximation Reynolds number: Inertial / Viscous forces Peclet number: Inertial / Diffusive Froude number: Inertial / Buoyancy (1/Fr = TI N) For inviscid flow, no diffusion of density, Re, Pe infinite
Is the flow unstable? Consider radially outward gravity
Comparison: Boussinesq (blue), non-Boussinesq (red) m = 2, = 0.1
Component equations Continuity equations Density evolution equations
Background literature: • Studying discontinuities of vorticity / densities or any passive scalar was initiated by Saffman who studies a random distribution of vortices as a model for 2D turbulence and predicted a k-4 spectrum • Bassom and Gilbert (JFM, 1988) studied spiral structures of vorticity and predicted that the spectrum lies between k-3 and k-4 • Pullin, Buntine and Saffman (Phys. Fluid, 1994) verify the Lundgren’s model of turbulence based on vorticity spiral
Batchelor (JFM, 1956) argued that at very large Reynolds number, the vorticity field inside closed streamlines evolves towards a constant value. • Rhines and Young (JFM, 1983) showed that any sharp gradients of a passive scalar will be homogenized at Pe1/3 • Bajer et al. (JFM, 2001) showed that the same holds true for the vorticity field, viz. thomo ~ Re1/3 • Flohr and Vassilicos (JFM, 1997) showed that a spiral structure unique among the range of vorticity distribution. Closed spaced spiral lead to an accelerated diffusion where Dk is the Kolmogorov capacity of the spiral
Navier-Stokes: Boussinesq approximation , radial gravity Density evolution Continuity