The haze was first observed by the Venera and Pioneer Venus probes in the 1970s, yet its composition remained an enigma. Planetary scientist Hiroki Karyu and his team employed a microphysical model to solve the mystery.
According to a study published in Nature Astronomy, 'shooting stars' burning up in the Venusian atmosphere leave behind cosmic dust. Sulfuric acid then interacts with these particles to create the persistent lower haze layer. Karyu stated in the study that the continuous influx of cosmic dust is sufficient to sustain the haze, matching the particle size distribution observed by entry probes decades ago.
The findings suggest these haze particles of cosmic origin act as efficient condensation nuclei, promoting cloud formation in the main cloud deck. The research resolves a long-standing question about the chemistry and dynamics of Venus' atmosphere.