Theory of magnetohydrodynamic waves: The WKB Approximation revisited
- 1 August 1992
- journal article
- research article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 97 (A8) , 12105-12112
- https://doi.org/10.1029/92ja00996
Abstract
Past treatments of the eikonal or WKB theory of the propagation of magnetohydrodynamic waves have assumed a strictly isentropic background. If in fact there is a gradient in the background entropy, then in second order in the WKB ordering, adiabatic fluctuations (in the Lagrangian sense) are not strictly isentropic in the Eulerian sense. This means that in the second order of the WKB expansion, which determines the variation of wave amplitude along rays, the violation of isentropy must be accounted for. The present paper revisits the derivation of the WKB approximation for small‐amplitude magnetohydrodynamic waves, allowing for possible spatial variation of the background entropy. The equation of variation of wave amplitude is rederived; it is a bilinear equation which, it turns out, can be recast in the action conservation form. It is shown that this action conservation equation is in fact equivalent to the action conservation law obtained from Lagrangian treatments (Dewar, 1970; Jacques, 1977a, b).This publication has 10 references indexed in Scilit:
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