Da. Gurnett et al., Non-detection at Venus of high-frequency radio signals characteristic of terrestrial lightning, NATURE, 409(6818), 2001, pp. 313-315
The detection(1,2) of impulsive low-frequency (10 to 80 kHz) radio signals,
and separate very-low-frequency (similar to 100 Hz) radio 'whistler' signa
ls(3-5) provided the first evidence for lightning in the atmosphere of Venu
s. Later, a small number of impulsive high-frequency (100 kHz to 5.6 MHz) r
adio signals, possibly due to lightning, were also detected(6). The existen
ce of lightning at Venus has, however, remained controversial(7-13). Here w
e report the results of a search for high-frequency (0.125 to 16 MHz) radio
signals during two close fly-bys of Venus by the Cassini spacecraft. Such
signals are characteristic of terrestrial lightning, and are commonly heard
on AM (amplitude-modulated) radios during thunderstorms. Although the inst
rument easily detected signals from terrestrial lightning during a later fl
y-by of Earth (at a global flash rate estimated to be 70 s(-1), which is co
nsistent with the rate expected for terrestrial lightning), no similar sign
als were detected from Venus. If lightning exists in the venusian atmospher
e, it is either extremely rare, or very different from terrestrial lightnin
g.