Ozone evolution and UV shielding in an oxygen-bearing Martian atmosphere
Develop and apply a one-dimensional photochemical model of the Martian atmosphere to resolve the outstanding questions about ozone evolution and determine whether an oxygen-bearing low-pressure Martian atmosphere would adequately moderate surface UV irradiance.
References
Simple models suggest that 20 mbar of oxygen would be sufficient to moderate Martian UV irradiance to present-day Earth values through the photochemical production of ozone, eg. The Ultraviolet Environment of Mars: Biological Implications Past, Present, and Future, Cockell et al. 2000. However, questions remain around the evolution of ozone in a Martian atmosphere, and 1-D photochemical modeling of the Martian atmosphere is needed to conclusively answer this question.
— An Introduction to Mars Terraforming, 2025 Workshop Summary
(2510.07344 - Stork et al., 7 Oct 2025) in Appendix, note 7