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It is shown that during certain years of intense nuclear testing, high-yield nuclear explosions seem to have injected into the stratosphere about 1034 nitric oxide molecules. (This is similar to estimates for NO generation from 500 SST flying for a year.) Large catalytic ozone reduction from such NO injection was not observed in worldwide total ozone measurements in the months following the explosions.
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Foley et al. (1973) studied this question.
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