Ozone is a major source of OH radicals in the troposphere.
It is
well-known that photodissociation of ozone is key for the conversion
of ozone into OH radicals. In the present study, using Born–Oppenheimer
molecular dynamics simulation, we have shown that on the surface of
the droplet and ice, ozone can dissociate without light. In addition,
the dissociation time of ozone is found to be much less on the ice
surface than the same time on the water droplet. As the dissociation
of ozone on the water surface can happen during the day as well as
in the night time, we believe this route of forming OH radicals can
be even more important than the photodissociation. The present study
suggests that the cloud and ice surface can enhance the oxidizing
power of the troposphere.