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It will be shown that the model chemistries used to calculate the effects of supersonic transports for Climatic Impact Assessment Program (Grobecker et al., 1975) and National Research Council (1975 a ) studies and of large‐scale nuclear exchanges for National Research Council (1975 b ) studies cause our one‐dimensional model to predict ozone depletions in 1963–1964 resulting from NO x injected into the stratosphere by the atmosphere nuclear tests of 1956–1962 larger (4–14% ozone reduction in 1963) than is easily consistent with observation. However, calculations carried out with more recent model chemistries result in ozone reductions that are more easily consistent with observation.
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Chang et al. (1979) studied this question.
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