Alfvén waves in a plane parallel flowing atmosphere

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Solar Wind Plasma, Sources Of Solar Wind, Magnetohydrodynamic Waves, Magnetohydrodynamic And Fluid Equation

Scientific paper

The present paper considers Alfvén waves in an inhomogeneous medium, under a non-uniform external magnetic field and in the presence of a non-uniform flow, to obtain the wave equations for the velocity and magnetic field perturbations in the case of propagation along a vertical uniform external magnetic field in an atmosphere with a vertical mean flow velocity and satisfying mass conservation. The wave equation has a critical layer where the mean flow velocity equals the Alfvén speed, and in the case of an isothermal atmosphere, the wave equation for the magnetic field perturbation can be reduced to a Bessel type with complex order and imaginary variable. Thus it is possible to obtain exact solutions for all frequencies and distances, discussing the cases in which there are propagating or evanescent waves far below or far above the critical layer, i.e., the latter acts as a reflecting layer. The solution in the vicinity of the critical layer allows the amplitude and phase of the wave field to be plotted, as a function of distance from the critical layer (measured in scale heights), for different values of the dimensionless frequency and initial Alfvén number (ratio of flow velocity to Alfvén speed). One application is the solar atmosphere, for which the MHD equations are appropriate, and the wavelengths are large compared with the density scale height, thus excluding the ray approximation. .

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