During the Galileo probe's descent through Jupiter's atmosphere, under
the ionosphere, the lightning and radio emission detector measured ra
dio frequency signals at levels significantly above the probe's electr
omagnetic noise. The signal strengths at 3 and 15 kilohertz were relat
ively large at the beginning oi the descent, decreased with depth to a
pressure level of about 5 bars, and then Increased slowly until the e
nd of the mission. The 15-kilohertz signals show arrival direction ani
sotropies. Measurements of radio frequency wave forms show that the pr
obe passed through an atmospheric region that did not support lightnin
g within at least 100 kilometers and more likely a few thousand kilome
ters of the descent trajectory. The apparent opacity of the jovian atm
osphere increases sharply at pressures greater than about 4 bars.