The plasma density and magnetic field are highly spatially and tempora
lly variable in the Venus nightside ionosphere. This variability may a
ffect the propagation and the generation of plasma waves. We determine
how these irregularities are related to plasma wave activity. Previou
sly, we have found two types of signals in the lower ionosphere, 100-H
z narrow-band signals and high-frequency wideband bursts. We investiga
te how these two different wave phenomena depend on the structure of t
he ionosphere. We calculate the ratios of the instantaneous values of
electron density, magnetic field, and electron temperature relative to
their average (1 min) values, and also their gradient scale lengths.
The 5.4-kHz burst activity is related to density depressions and obvio
us electron temperature enhancements, tint varies little with magnetic
field strength. The 100-Hz narrow-band signals are often associated w
ith significantly enhanced magnetic field and depressions of electron
density. Both higher field strength and lower density result in a lowe
r beta (ratio of thermal pressure to magnetic pressure) plasma, which
favors the propagation of whistler waves. We find that neither type of
signal is associated with gradients of the magnetic field, but the 5.
4-kHz wideband Signals have higher occurrence rates at higher electron
density and temperature gradients, while the 100-Hz harrow-band burst
rate increases only slightly for steeper gradients. A local gradient-
driven instability cannot explain most of the 100-Hz narrow-band signa
ls, but some 5.4-kHz signals may be associated with pressure gradients
.