Howell C D, Michelangeli D V, Allen M, Yung Y L
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena 91125, USA.
Planet Space Sci. 1990 Apr;38(4):529-37. doi: 10.1016/0032-0633(90)90145-g.
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.
报告了太阳中层探测器(SME)在北纬45度对1984年7月10日至31日期间凌晨3点1.27微米夜辉的观测结果。根据推导的体积发射率,我们得出了80 - 100千米高度范围内O2(a1Δg)的夜间产生率。利用SME在同一纬度和时间段获取的下午3点的平均臭氧剖面以及一个更新的光化学模型,我们确定了夜间O、O3、H、OH、HO2和H2O2的剖面。这些用于计算那些放热足够多以产生O2(1Δ)或OH或HO2的激发态的反应速率,这些激发态可以将其能量转移给O2以形成O2(1Δ)。在这些反应中,大多数反应速率与观测到的夜间O2(1Δ)产生率相比非常小。对于其他几个反应,实验室实验发现O2(1Δ)的产率不足以模拟观测到的O2(1Δ)。基于已发表的实验室和观测研究使用O2(1Δ)的产率,我们发现两个反应序列的总和可以近似SME的测量结果:(1)O + O + M和(2)H + O3,随后是OH* + O2。