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Paper: Characterizing Proterozoic Earth-like Planets in the Near Ultraviolet with HWO
Monograph: 11, HWO25 Proceedings Part II: Mission Framework, Technology, and Broader Contributions
Page: 137
Authors: Amber V. Young, Giada Arney, Tyler D. Robinson, Shawn D. Domagal-Goldman, Roser Juanola-Parramon, Christopher C. Stark, Renyu Hu, Armen Tokadjian, and Mario Damiano
DOI: 10.26624/XONA6638
Abstract: Detecting biosignatures on Proterozoic Earth-like exoplanets requires sensitivity to near ultraviolet (NUV) spectral features, particularly ozone (O3), which serves as a proxy for molecular oxygen (O2) in atmospheres where direct detection is challenging. Using photochemical-climate modeling and retrieval simulations, we assess the observational requirements for robust O3 detection and the potential for spectral false positives from sulfur dioxide (SO2). Our results show that O3 abundances as low as 0.1% of present atmospheric levels can be constrained to within an order of magnitude at 1 σ confidence using three adjacent photometric bandpasses, each with a 15% width, and a short wavelength cutoff for those observations near 0.26 µm. The self-consistent steady state atmospheric modeling results show that SO2 buildup is difficult in a habitable environment with appreciable amounts of water vapor in its atmosphere and would require volcanic outgassing rates at least two orders of magnitude above present-day Earth to reach surface abundance levels comparable to Proterozoic Earth-like abundances of O3. Even under these high SO2 flux scenarios, SO2 remains largely unconstrained with the recommended observational configuration. These findings support the inclusion of UV coronagraph instrumentation on HWO to enable biosignature detection strategies that are sensitive to atmospheric conditions spanning key phases of Earth's geological history.
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