Galileo has been in orbit around Jupiter since December 1995. All the orbit
s are equatorial and elliptical, with apogees between 60 R-J - 142 R-J and
perigees from 8 - 12 R-J. Since orbit injection, the plasma wave instrument
(PWS) has been collecting data over specific intervals of each of the orbi
ts at all local times and a range of different radial distances. We present
the results of a survey of the data for the frequency range 300 kHz to 5.6
MHz, which includes the hectometric (HOM) and low-frequency decametric (DA
M) emissions. The results indicate that both the HOM and DAM emission are m
ore intense and occur more frequently in the midnight sector of Jupiter. Th
is is in analogy to Earth and consistent with a magnetic substorm source fo
r a portion of the radio emissions in this frequency range. Another peak in
the power levels is observed on the Jovian dayside in the local time range
11 hrs. < LT < 12 hrs. This peak does not have a terrestrial counterpart.
We speculate that this dayside peak may be a result of sampling near perige
e, but we cannot rule out the possibility that this is not the case.