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Fig. 1

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Relationship between NOx and HOx in the lower atmosphere on modern Earth, adapted from Logan et al. (1981). In the NOx-limited regime (white background) an increase of NOx will lead to an increase of HOx and thus increased productivity of the smog mechanism. In the ΝΟx-saturated regime (gray background) the NOx/HOx ratio reaches a tipping point where NOx begins to deplete HOx by locking it up into stable reservoir species, therefore suppressing smog formation.

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