AN ANALYSIS OF WHISTLER WAVES AT
INTERPLANETARY SHOCKS
LENGYELFREY D
FARRELL WM
STONE RG
BALOGH A
FORSYTH R
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
v.99, n.A7, JUL 1, 94, p.13325-13334
We present an analysis of whistler wave magnetic and electric field amplitude
ratios from
which we compute wave propagation angles and energies of electrons in
resonance with the
waves. To do this analysis, we compute the theoretical dependence of ratios
of wave
components on the whistler wave propagation angle theta for various
combinations of
orthogonal wave components. Ratios of wave components that would be observed
by a
spinning spacecraft are determined, and the effects of arbitrary inclinations
of the spacecraft to
the ambient magnet ic field and to the whistler wave vector are studied. This
analysis clearly
demonstrates that B/E, the ratio of magnetic to electric field amplitudes,
cannot be assumed to
be the wave index of refraction, contrary to assumptions of some earlier
studies. Therefore
previous interpretations of whistler wave observations based on this
assumption must be
reinvestigated. B/E ratios derived usi ng three orthogonal wave components
can be used to
unambiguously determine theta. Using spin plane observations alone, a
significant uncertainty
occurs in the determination of theta. Nevertheless, for whistler waves
observed downstream
of several interplanetary shocks by the Ulysses plasma wave experiment we fi
nd that theta
is highly oblique. We suggest that the analysis of wave amplitude ratios used
in conjunction
with traditional stability analyses provide a promising tool for determining
which particle
distributions and resonances are likely to be dominant contributors to wave
growth.