Ashen light

Hypothesised glow in Venus's light
the similar appearance with the Earth's moon

Ashen light is a hypothesised subtle glow that has been claimed to be seen on the night side of the planet Venus. The phenomenon has not been scientifically confirmed, and theories as to the observed phenomenon's cause are numerous, such as emission of light by Venus, or optical phenomena within the observing telescope itself. A modern hypothesis as to the source of light on Venus suggests it to be associated with lightning,

While the discovery of the ashen light is often attributed to Italian astronomer Giovanni Battista Riccioli, recent evidence finds that German priest Athanasius Kircher might have been the first to observe the ashen light during his one and only trip to Palermo, Sicily in the spring of 1638. However, the first distinct and detailed record of the ashen light was produced by Riccioli on 9 January 1643, who ascribed it to the refraction of light within the telescope itself: "The colors arise from the various refraction of light in the glass, as it happens with trigonal glasses." This is likely a description of a phenomenon now known as chromatic aberration. Subsequent claims have been made by various observers ever since, including Sir William Herschel, Sir Patrick Moore, Dale P. Cruikshank, and William K. Hartmann. The ashen light has often been sighted when Venus is in the evening sky, when the evening terminator of the planet is toward the Earth. Observation attempts were made on 17 July 2001, when a 67% illuminated Venus reappeared from behind a 13% illuminated moon. None of the observers of this occurrence (including some using 'Super RADOTS' telescopes) reported seeing the ashen light. Video from the event was captured, but the camera was too insensitive to detect even the earthshine. A particularly favourable viewing opportunity occurred on 8 October 2015, with a 40% illuminated Venus reappearing from behind the unlit limb of a 15% sunlit Moon. The event was visible in dark skies throughout Central Australia and was recorded by David and Joan Dunham (of the International Occultation Timing Association) using a 10" f/4 Newton telescope with a Watec 120N+ video camera from a location just north of Alice Springs. They also observed the event visually with an 8" Schmidt–Cassegrain telescope. Neither the real time visual observation nor close visual inspection of the video recording showed any sign of the dark side of Venus.

The Keck telescope on Hawaii reported seeing a subtle green glow and suggested it could be produced as ultraviolet light from the Sun splits molecules of carbon dioxide (CO2), known to be common in Venus' atmosphere, into carbon monoxide and oxygen However, the green light emitted as oxygen recombines to form is thought too faint to explain the effect,

In 1967, Venera 4 found the Venusian magnetic field to be much weaker than that of Earth. This magnetic field is induced by an interaction between the ionosphere and the solar wind, rather than by an internal dynamo in the core like the one inside Earth. Venus's small induced magnetosphere provides negligible protection to the atmosphere against cosmic radiation. This radiation may result in cloud to cloud lightning discharges. It was hypothesized in 1957 by Urey and Brewer that CO+, CO and O ions produced by the ultraviolet radiation from the Sun were the cause of the glow. In 1969, it was hypothesized that the Ashen light is an auroral phenomena due to solar particle bombardment on the dark side of Venus. Throughout the 1980s, it was thought that the cause of the glow was lightning on Venus. The Soviet Venera 9 and 10 orbital probes obtained optical and electromagnetic evidence of lightning on Venus. Also, the Pioneer Venus Orbiter recorded visible airglow at Venus in 1978 strong enough to saturate its star sensor. The Akatsuki spacecraft, by Japan's space agency JAXA, entered orbit around Venus on 7 December 2015. Part of its scientific payload includes the Lightning and Airglow Camera (LAC) which is looking for lightning in the visible spectrum (552 777 nm). To image lightning, the orbiter has sight of the dark side of Venus for about 30 minutes every 10 days. No lightning has been detected in 16.8 hours of night side observation (July 2019). Simulations indicate that the lightning hypothesis as the cause of the glow is incorrect, as not enough light could be transmitted through the atmosphere to be seen from Earth. Observers have speculated it may be illusory, resulting from the physiological effect of observing a bright, crescent shaped object. Spacecraft looking for it have not been able to spot it — leading some astronomers to believe that it is just an enduring myth.