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On the stability of heterogeneous shear flows

1961/06/01 by John W. Miles · 33 citations
Earth and Planetary Sciences · Mathematics · Environmental Science · #Aquatic and Environmental Studies #Navier-Stokes equation solutions #Methane Hydrates and Related Phenomena

paper · doi:10.1017/s0022112061000305

Abstract

Small perturbations of a parallel shear flow U(y) in an inviscid, incompressible fluid of variable density ρ 0 (y) are considered. It is deduced that dynamic instability of statically stable flows ( ρ 0 (y) \textless 0 ) cannot be other than exponential, in consequence of which it suffices to consider spatially periodic, travelling waves. The general solution of the resulting differential equation is considered in some detail, with special emphasis on the Reynolds stress that transfers energy from the mean flow to the travelling wave. It is proved (as originally conjectured by G. I. Taylor) that sufficient conditions for stability are U(y) \not= 0 and J(y) \textgreater \frac 1 4 throughout the flow, where J(y) = -g ρ0(y)|ρ (y)U′ 2(y) is the local Richardson number. It also is pointed out that the kinetic energy of a normal mode in an ideal fluid may be infinite if 0 \textless J(yc) \textless \frac 14 , where U(yc) is the wave speed.

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