Bt. Tsurutani et al., THE RELATIONSHIP BETWEEN INTERPLANETARY DISCONTINUITIES AND ALFVEN WAVES - ULYSSES OBSERVATIONS, Geophysical research letters, 21(21), 1994, pp. 2267-2270
The rate of occurrence of interplanetary discontinuities (ROID) is exa
mined using Ulysses magnetic field and plasma data from 1 to 5 AU radi
al distance from the Sun and at high heliographic latitudes. We find t
wo regions where the ROID is high: in stream-stream interaction region
s and in Alfven wave trains. This latter feature is particularly obvio
us at high latitudes when Ulysses enters a high speed stream associate
d with a polar coronal hole. These streams are characterized by the pr
esence of continuous, large-amplitude (DELTAB/\B\ approximately 1-2) A
lfven waves and an extraordinarily high ROID value (approximately 150
discontinuities/day). In a number of intervals examined, it is found t
hat (rotational) discontinuities are an integral part of the Alfven wa
ves. The nonlinear Alfven waves are spherically polarized, i.e., the t
ip of the perturbation vector resides on the surface of a sphere (a co
nsequence of constant \B\). The slowly rotating part of the waves rota
tes approximately 270-degrees in phase. There is a slight arc in the B
1-B2 hodogram, suggesting an almost linear polarization. The phase rot
ation associated with the discontinuity is approximately 90-degrees, l
ies in the same plane as the slowly rotating part of the Alfven wave,
and therefore completes the 360-degrees phase rotation. The best descr
iption of the overall Alfven wave plus discontinuity is a spherical, a
rc-polarized, phase-steepened wave.