Confirm the H2S detection and sulfur-enrichment interpretation for HAT-P-1 b
Determine whether HAT-P-1 b truly hosts detectable hydrogen sulfide (H2S) and whether its sulfur abundance can be used as a tracer of refractory-to-volatile enrichment by obtaining observations that jointly constrain the 1.4 μm H2O band, the 3–4 μm sulfur-sensitive region, and the 4.3 μm CO2 band.
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We caution, however, that the present \ce{H2S} inference remains tentative. Due to the relatively small feature size compared to the pronounced, broader \ce{H2O} and \ce{CO2} opacities present, the \ce{H2S} measurement is more vulnerable to instrument systematics. In addition, \ce{H2S} is photochemically coupled to other sulfur-bearing-species, especially \ce{SO2}, and overlapping opacities between these species can complicate retrieved abundance estimates \citep{Tsai2023}. Future observations that jointly constrain the 1.4~$\mu$m \ce{H$_2$O} band, the 3-4~$\mu$m sulfur-sensitive region, and the 4.3~$\mu$m \ce{CO$_2$} band will be needed to determine whether HAT-P-1 truly hosts detectable \ce{H2S} and whether its sulfur abundance can be used as a tracer of refractory-to-volatile enrichment.