Auroral implications of recent measurements on O(1S) and O(1D) formation in the reaction of N(+) with O2

Physics

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Atmospheric Chemistry, Auroral Zones, Emission Spectra, Oxygen Afterglow, Reaction Kinetics, Nitrogen Ions, Oxygen

Scientific paper

Recent flowing afterglow measurements have shown that the reaction of N(+) with O2 produces 70 + or - 30 percent of the oxygen atom product as O(1D) and less than 0.1 percent as O(1S). These results indicate that this reaction does not contribute to the auroral green line emission (5577 A), but can account for about 10 percent of the observed red line (6300 A) auroral emission.

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