71 6 Encyclopedia of the Solar System
(b)
(a) FIGURE^21 (a) Dynamic spectra
of Saturn’s SKR emission. This
illustrates a dramatic intensification
of the SKR in response to an
interplanetary shock that passed
Cassiniat about 20:30 on June 8,
- (b) A high temporal and
spectral resolution record of SKR
obtained byCassini. This
spectrogram illustrates the complex
structure and variations in the SKR
spectrum, which is also typical of
cyclotron maser emissions at Jupiter
and Earth. (After Kurth, et al.,
2005, High Spectral and Temporal
Resolution Observations of Saturn
Kilometric Radiation.Geophys.
Res. Lett. 32 , L20S07,
doi:1029/2005 GL022648.)
shadowing conditions to theVoyagerera late inCassini’s
orbital tour, so such speculation can be tested.
3.7 Uranus and Neptune
Like Saturn’s radio emissions, both smooth and bursty com-
ponents are apparent in the radio emissions from Uranus
and Neptune, and these emissions probably originate in the
southern auroral regions of the planets. Note, though, that
the magnetic fields of these planets are inclined by large
angles (47◦for Uranus, 59◦for Neptune) with respect to
their rotational axes, and hence the auroral regions are not
near the rotation poles. The periodicity of the emissions
leads to the determination of the rotation periods of both