" Absorption cross sections from DeMore et al. (1997) recommendation based on Ravishankara and Mauldin (1986), Sander (1986), and Canosa-Mas et al. (1987); quantum yields Irom Johnston et al. (1996).

It is this process, followed by reaction (21a)

that is primarily responsible for the production of reactive oxides of nitrogen in the stratosphere in a "natural" atmosphere (see Chapter 12).

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