This paper considers Alfvén waves in a radially stratified medium
where all background quantities, namely mass density, magnetic field strength
and mean flow velocity, depend only on the distance from the centre, the latter
two being assumed to lie in the radial direction. It is shown that the radial
dependence of Alfvén waves is the same for two cases: (i) when the velocity and
magnetic field perturbations are along parallels, in the one-dimensional case of
only radial and time dependence; (ii) in the three-dimensional case with
dependence on all three spherical coordinates and time, for velocity and
magnetic field perturbations with components along parallels and meridians,
represented by the radial components of the vorticity and electric current
respectively. Elimination between these equations leads to the convected
Alfvén-wave equation in the case of uniform flow, and an equation with an
additional term in the case of non-uniform flow with mean flow velocity a linear
function of distance. The latter case, namely that of non-uniform flow with flow
velocity increasing linearly with distance, is analysed in detail; conservation of
mass flux requires the mass density to decay as the inverse cube of the distance.
The Alfvén-wave equation has a critical layer where the flow velocity equals the
Alfvén speed, leading to three sets of two solutions, namely below, above and
across the critical layer. The latter is used to specify the wave behaviour in the
vicinity of the critical layer, where local partial transmission occurs. The
problem has two dimensionless parameters: the frequency and the initial
Alfvén number. It is shown, by plotting the wave fields relative to the critical
layer, that these two dimensionless parameters appear in a single combination.
This simplifies the plotting of the wave fields for several combinations of
physical conditions. It is shown in the Appendix that the formulation of the
equations of MHD in the original Elsässer (1956) form, often used in the recent
literature, does not apply if the background mass density is non-uniform on the
scale of a wavelength. The present theory, based on exact solutions of the
Alfvén-wave equation for a inhomogeneous moving medium, is unrestricted as
to the relative magnitude of the local wavelength and scale of change of
properties of the background medium. The present theory shows that the rate-of-decay of wave amplitude is strongly dependent on wave frequency beyond
the critical layer, i.e. the process of change with distance of the spectrum of
Alfvén waves in the solar wind starts at the critical layer.