Photolytic Hazes in the Atmosphere of 51 Eri b
Kevin J. Zahnle, Mark S. Marley, Caroline V. Morley, Julianne I. Moses

TL;DR
This study models photochemistry in 51 Eri b's atmosphere, revealing sulfur photochemistry's importance and predicting sulfur cloud formation, with implications for a wide range of exoplanets.
Contribution
It introduces a detailed 1D photochemical model highlighting sulfur's role and predicts sulfur cloud formation, expanding understanding of atmospheric processes on warm Jupiters.
Findings
Sulfur photochemistry converts H₂S into elemental sulfur (S₈).
Condensed sulfur clouds form in cooler models below 700 K.
Vapor sulfur species are observable in warmer models.
Abstract
We use a 1D model to address photochemistry and possible haze formation in the irradiated warm Jupiter, 51 Eridani b. The intended focus was to be carbon, but sulfur photochemistry turns out to be important. The case for organic photochemical hazes is intriguing but falls short of being compelling. If organic hazes form, they are likeliest to do so if vertical mixing in 51 Eri b is weaker than in Jupiter, and they would be found below the altitudes where methane and water are photolyzed. The more novel result is that photochemistry turns HS into elemental sulfur, here treated as S. In the cooler models, S is predicted to condense in optically thick clouds of solid sulfur particles, whilst in the warmer models S remains a vapor along with several other sulfur allotropes that are both visually striking and potentially observable. For 51 Eri b, the division between models…
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