Ion collisions in plasmas cause damping of hydromagnetic modes,
but also a strong Hall effect if the collision time is of the same order as
the gyroperiod.
This is known to be very marked in the E region of the Earth's
ionosphere, but
should also occur in other partially ionized space and laboratory
plasmas. In this work dynamic effects of such Hall currents are investigated
theoretically. The linear modes that are obtained are, for sufficiently
large scales, distinctly
different from ordinary damped Alfvén modes, and similar to
whistler waves even when the dynamic time scale is much longer than the ion
gyroperiod. The
dynamics of the coupling between planetary ionospheres and magnetospheric
plasmas may be viewed as a reflection of Alfvén waves at a
sharp boundary. By
applying the results of the linear mode analysis, it is shown
that the usually employed reflection coefficient needs to be replaced by a
reflection tensor for
large-scale waves due to self-induction of ionospheric Hall currents.
This is similar to the magneto-optical Kerr effect, which is well-known in
solid state physics. In the Earth's ionosphere, variations from
incident torsional modes
over periods as long as several minutes, which have been observed to
occur over scales of a few thousand kilometres, are predicted to cause the
generation of substantial eddy electric fields and compressional flows.
Consequences for the
energy exchange between ionosphere and magnetosphere and possibilities to
observe the effect are discussed.