Fig. 1

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Impact of HO2 and OH in the NOx-limited and NOx-saturated regimes on modern Earth, adapted from Logan et al. (1981). In the NOx-limited regime (white background), increasing NOx allows for a more efficient smog mechanism, with the resulting increase in O3 causing a corresponding rise in HOx. In the NOx-saturated regime (gray background), the abundance of NOx rises to the point where smog O3 production is suppressed as NOx depletes HOx (a necessary catalyst for the smog mechanism) by locking it up into reservoir species.
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