Conservation laws that relate the local time-rate-of-change of the spatial integral of a density function to the divergence of its flux through the boundaries of the integration domain provide integral constraints on the spatio-temporal development of a field. Here we show that a new type of conserved quantity exists that does not require integration over a particular domain but which holds locally at any point in the field. This is derived for the pseudo-energy density of non-divergent Rossby waves where local invariance is obtained for (i) a single plane wave, and (ii) waves produced by an impulsive point source of vorticity. The definition of pseudo-energy used here consists of a conventional kinetic part, as well as an unconventional ps...
A class of exact solutions of the equation of conservation of the quasi-geostrophic vorticity in a c...
Traditional derivations of available potential energy, in a variety of contexts, involve combining s...
AbstractLet u be a classical solution to the wave equation in an odd number n of space dimensions, w...
Conservation laws that relate the local time-rate-of-change of the spatial integral of a density fun...
We consider an adiabatic-type (approximate) invariant that was earlier obtained for the quasi-geostr...
The evolution of wave energy, enstrophy, and wave motion for atmospheric Rossby waves in a variable ...
The Earth’s atmosphere and oceans contain strongly swirling coherent structures. The sphericity of ...
A variational principle for Rossby waves in beta-plane approximation is formulated. Special attentio...
AbstractHomogeneous wave equations satisfied by the 4-vector momentum density p(including the mass-e...
Explicit expressions of the 3D velocity field in terms of the conserved quantities of ideal fluid th...
We calculate the net instantaneous power exchanged between two sets of modes in a generic system gov...
Abstract For mid-latitude Rossby waves (RWs) in the atmosphere, the expression for the energy flux f...
International audienceWe propose an analytical solution for the evolution of the spatial variability...
Oceanic Rossby waves and eddies flux energy and fluid westward, the latter through the Stokes drift ...
Some properties of one-dimensional potential waves are discussed. In particular it is shown that wav...
A class of exact solutions of the equation of conservation of the quasi-geostrophic vorticity in a c...
Traditional derivations of available potential energy, in a variety of contexts, involve combining s...
AbstractLet u be a classical solution to the wave equation in an odd number n of space dimensions, w...
Conservation laws that relate the local time-rate-of-change of the spatial integral of a density fun...
We consider an adiabatic-type (approximate) invariant that was earlier obtained for the quasi-geostr...
The evolution of wave energy, enstrophy, and wave motion for atmospheric Rossby waves in a variable ...
The Earth’s atmosphere and oceans contain strongly swirling coherent structures. The sphericity of ...
A variational principle for Rossby waves in beta-plane approximation is formulated. Special attentio...
AbstractHomogeneous wave equations satisfied by the 4-vector momentum density p(including the mass-e...
Explicit expressions of the 3D velocity field in terms of the conserved quantities of ideal fluid th...
We calculate the net instantaneous power exchanged between two sets of modes in a generic system gov...
Abstract For mid-latitude Rossby waves (RWs) in the atmosphere, the expression for the energy flux f...
International audienceWe propose an analytical solution for the evolution of the spatial variability...
Oceanic Rossby waves and eddies flux energy and fluid westward, the latter through the Stokes drift ...
Some properties of one-dimensional potential waves are discussed. In particular it is shown that wav...
A class of exact solutions of the equation of conservation of the quasi-geostrophic vorticity in a c...
Traditional derivations of available potential energy, in a variety of contexts, involve combining s...
AbstractLet u be a classical solution to the wave equation in an odd number n of space dimensions, w...