The first observation of possible transient luminous events (TLEs) on Jupiter was recently reported by Giles et al. (2020). This is a finding that resembles the serendipitous capture of Earth's TLEs on camera three decades ago (Franz et al., 1990). Specifically, the ultraviolet spectrograph (UVS) aboard the Juno spacecraft has recorded 11 optical signals during the first 4 years of the mission that may have originated from TLEs on Jupiter. Light curves for 10 of the flashes show a mean decay time of ∼1.4 ms while the remaining flash has a noticeably shorter duration (i.e., 0.1 ms), which possibly may be because Juno's UVS was triggered immediately before the photodetector moved off the flash. Additional properties of the detected flashes and the observation geometry may be found in Giles et al. (2020, Table 1). 2020) use a model of radiative transfer in Jupiter's atmosphere to locate the altitude of flashes. It is concluded that the best fit to the recorded spectrum of flashes is obtained for a source altitude of ∼258 km above the 1-bar level (i.e., ∼10 μbar pressure). Giles et al. ( 2020) emphasize that UV observations cannot probe altitudes below that corresponding to 100 mbar. As such, the UV signature of lightning, which is generally thought to occur at ∼5 bar and even the recently observed "shallow lightning" (Becker et al., 2020) that occurs at pressures higher than 1.4 bar will be absent from Juno UVS observations (e.g., Moses et al., 2005, Figure 8). It is therefore clear that Giles et al. (2020) did not observe typical lightning discharges.
Giles et al. (Previous observations of Jupiter lightning were limited by camera sensitivity, distance from Jupiter and long exposures. This contributed to the exclusive detection of Jupiter lightning with optical energies comparable to terrestrial superbolts (e.g., Turman, 1977) (i.e., ∼10 9 J). Juno's observations of Jupiter, however, has led to the conclusion that Jupiter lightning predominantly consists of flashes with optical energies similar to typical terrestrial energies (i.e., 10 5 -10 8 J) (Becker et al., 2020, Figure 2). Kolmašová et al. (2018) report a much higher lightning frequency, which is comparable to the frequency of lightning on Earth, and Becker et al. (2020) report an increase in the flash rate from ∼4 × 10 −3 to ∼6.1 × 10 −2 flashes per square kilometer per year with several flashes