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Two‐dimensional model calculations have been carried out of the distributions of the fluorine‐containing reservoir species HF, CF 2 O, and CFClO. HF constitutes the largest fluorine reservoir in the stratosphere, but CF 2 O also makes an important contribution to the inorganic fluorine budget. CFClO amounts are most important in the tropical lower stratosphere. HF amounts increase with altitude throughout the stratosphere, while those of CF 2 O and CFClO fall off above their mixing ratio peaks due to photolysis. The model is in good qualitative agreement with observed vertical profiles of HF arid CF 2 O but tends to underestimate the total column of HF. The calculated CFClO distribution is in good agreement with the very limited data. The disagreement in the HF columns is likely due to small inaccuracies in the model's treatment of lower stratospheric photolysis of chlorofluorocarbons. The model results support the suggestion that CF 2 O may be heterogeneously converted to HF on the surface of polar stratospheric cloud particles. The model results also suggest that the quantum yield for photolysis of CF 2 O is near unity.
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Kaye et al. (1991) studied this question.
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