Abstract
In order to describe the spectrum (or eigenvalues) of the reduced operator of stability (14.1′), (14.2′) in the complex plane, it is usually useful to study the properties of its quadratic form, a well-known method in the theory of linear operators in a Hilbert space. In the framework of linear theory we begin with a rigorous proof of the Miles stability criterion for a flow of a stratified fluid.
Theorem 16.1 (Miles 1961) A plane-parallel flow of a stratified fluid with its Richardson number
is stable.
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Notes
- 1.
V.P. Dymnikov drew the author’s attention to the following circumstance. In fact, the so-called formal stability of a shear flow proved above is based on the formal application of the stability criterion for finite-dimensional dynamical systems to systems with infinite number of degrees of freedom. The vanishing of the first variation and the positivity of the second variation, generally speaking, do not provide the minimum of the Lyapunov function (A.N. Filatov, Stability Theory, INM RAS, Moscow, 2002).
References
L.A. Dikii, Hydrodynamic Stability and the Dynamics of the Atmosphere, Gidrometeoizdat, Leningrad, 1976.
R. Fjortoft, Application of integral theorems in deriving criteria of stability for the baroclinic circular vortex. Geophys. Publ., Vol. 17, No. 2, 1950, Oslo.
L.N. Howard, Note on a paper of John Miles. J. Fluid Mech., Vol. 10, No. 2, 1961.
J.W. Miles, On the Stability of Heterogeneous Shear Flows. J. Fluid Mech., Vol. 10, No. 2, 1961.
J.W. Miles, Richardson’s criterion for the stability of stratified shear flows. Phys. Fluids, Vol. 29, No. 10, 1986.
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Dolzhansky, F.V. (2013). Applications of Integral Relations and Conservation Laws in the Theory of Hydrodynamic Stability. In: Fundamentals of Geophysical Hydrodynamics. Encyclopaedia of Mathematical Sciences, vol 103. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-31034-8_16
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DOI: https://doi.org/10.1007/978-3-642-31034-8_16
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