Publication Date:
2019-06-28
Description:
The first simultaneous measurements of HO(x), NO(x), and Cl(x) radicals in the middle stratosphere show that NO(x) catalytic cycles dominate loss of ozone (O3) for altitudes between 24 and 38 km; Cl(x) catalytic cycles are measured to be less effective than previously expected; and there is no 'ozone deficit' in the photochemically dominated altitude range from 31 and 38 km, contrary to some previous theoretical studies.
Keywords:
Geophysics
Type:
NASA-CR-200684
,
NAS 1.26:200684
Format:
application/pdf
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