Rj. Wilson et Mk. Dougherty, Evidence provided by Galileo of ultra low frequency waves within Jupiter'smiddle magnetosphere, GEOPHYS R L, 27(6), 2000, pp. 835-838
The Voyager and Ulysses spacecraft measurements from the dayside of Jupiter
's middle magnetosphere provided evidence for ultra low frequency waves in
the magnetometer data, in particular waves of periods 10 - 20 minutes. Gali
leo is the first orbiter mission around Jupiter and the,first to extensivel
y study the nightside magnetosphere. Similar waves are discernible when Gal
ileo passed through the equatorial current sheet with very few features bei
ng noticed outside of the current sheet regions. An overview of the data sh
ows that only 12% of crossings do not have any wave signatures in any compo
nent of magnetic field in the 10 - 20 minute period regime. The majority of
these waves are found in the perpendicular field component. These waves ar
e thus prevalent over the nightside magnetosphere and when combined along w
ith the earlier work on the dayside seems to suggest that these ultra low f
requency waves are a global phenomenon.