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Resonant Interaction of Rossby Waves; Helmholtz and Obukhov Singular Vortices; The Kirchhoff Equations

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Fundamentals of Geophysical Hydrodynamics

Part of the book series: Encyclopaedia of Mathematical Sciences ((EMS,volume 103))

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Abstract

The theory of wave processes tells us that the energy of waves of any nature propagates not with the phase velocity but with the group velocity

$$ \mathbf{C}_{gr}=\nabla_{\mathbf{k}}\omega,\quad \omega=\omega ( \mathbf{k} ), $$

where ω(k) is the dispersion relation for waves of this nature, and ∇ k is the gradient operation in the k-space of wave numbers. The waves whose phase velocity does not coincide with the group velocity are called dispersion waves. So, for instance, are gravitational-gyroscopic waves with the dispersion relation (7.20), according to which they isotropically propagate in space.

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Dolzhansky, F.V. (2013). Resonant Interaction of Rossby Waves; Helmholtz and Obukhov Singular Vortices; The Kirchhoff Equations. In: Fundamentals of Geophysical Hydrodynamics. Encyclopaedia of Mathematical Sciences, vol 103. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-31034-8_8

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