SME observations of O2 (1 delta g) nightglow:  an assessment of the chemical production mechanisms.
Solar Mesosphere Explorer (SME) observations of the 3 a.m. 1.27 micrometers nightglow at 45 N latitude, averaged over the period 10-31 July 1984, are reported.  From the deduced volume emission rates, we derive the O2(a1 delta g) night-time production rates for the 80-100 km altitude range.  Utilizing the mean SME-acquired 3 p.m. ozone profile for the same latitude and time period and an updated photochemical model, we determine night-time O, O3, H, OH, HO2, and H2O2 profiles.  These are used in calculating the rates of reactions which are sufficiently exothermic to produce O2(1 delta) or excited states of OH or HO2, which could transfer their energy to O2 to form O2(1 delta).  Of these reactions, most have rates that are quite small compared with the observed night-time O2(1 delta) production rate.  For several others, laboratory experiments have found O2(1 delta) yields which are insufficient for simulating the observed O2(1 delta).  Using yields of O2(1 delta) based on published laboratory and observational studies, we find that the sum of two reaction sequences can approximate the SME measurements:  (1) O+O+M and (2) H+O3 followed by OH*+O2.
Howell
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Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena 91125, USA.
Michelangeli
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Allen
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Yung
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D001272:Atmosphere / Q000032:analysis / Q000737:chemistry*; D003624:Darkness; D018534:Earth, Planet; D006859:Hydrogen / Q000737:chemistry; D008433:Mathematics; D008956:Models, Chemical; D010100:Oxygen / Q000737:chemistry*; D010777:Photochemistry; D018531:Spacecraft / Q000295:instrumentation*; D019265:Spectroscopy, Near-Infrared
D006859:Hydrogen; D010100:Oxygen