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Magnetohydrodynamic wavehyphen;current system with constant vorticity

机译：Magnetohydrodynamic wavehyphen;current system with constant vorticity

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The basic linear theory is given for a perfectly conducting stratified wave‐current system in which there is an upper layer of incompressible fluid of constant vorticity propagating on a slightly heavier lower layer of stagnant fluid. An extraneous homogeneous horizontal magnetic fieldB0is present, directed either longitudinally or transversely. Because of the magnetic field the basic governing equations for the system form a set ofdifferentialequations, in marked contrast to the single algebraic dispersion equation that would result were the magnetic field absent. The differential equations are solved, and the solutions are shown graphically for various cases of the magnetic field strength. ©1996 American Institute of Physics.

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