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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.

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Background

Accurate assessment of surface UV conditions under a terraformed, oxygen-bearing Martian atmosphere requires understanding ozone production and loss. While simple models suggest low levels of oxygen could yield sufficient ozone to protect the surface, the dynamics and stability of ozone under Martian conditions remain unresolved.

The authors highlight the need for targeted photochemical modeling to conclusively assess whether ozone would evolve to provide adequate UV shielding.

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