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- W2023095589 abstract "Comparison of previous theoretical work with observational data has suggested a downward NO flux through the mesopause on the order of (1–5)×108 cm−2 sec−1. The importance of this flux as a source of odd nitrogen in the mesosphere and upper stratosphere is investigated. Odd-nitrogen concentrations are found to be sensitive functions of the dissociation rate of NO and the odd-nitrogen flux into the lower stratosphere. It is highly improbable that NO is mixed in the mesosphere because predissociation of NO in the δ(0, 0) band results in a large NO dissociation rate throughout this region. The dissociation of NO to produce N(4S) and the subsequent reaction of N(4S) with NO results in a reduction of the odd-nitrogen flux from its mesopause value to approximately 106 cm−2 sec−1 at the stratopause." @default.
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- W2023095589 date "1971-12-01" @default.
- W2023095589 modified "2023-09-23" @default.
- W2023095589 title "Odd nitrogen in the mesosphere" @default.
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- W2023095589 doi "https://doi.org/10.1029/ja076i034p08384" @default.
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