The effect of reactants vibrational and rotational excitation on products (HO 2 + O and O 3 + H) formation is investigated for the title reaction by using the quasiclassical trajectory method and the realistic double many-body expansion (DMBE) potential energy surface for ground-state HO 3 . It is shown that it can be a potential source of ozone in the upper atmosphere.
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Caridade et al. (2001) studied this question.
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