振动激发的分子氮对中大气高度O3和N2O气体红外发射的影响

A. Kirillov, V. Belakhovsky
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引用次数: 0

摘要

计算了能量为E = 2,4,10 MeV的电子在地球中部大气30 ~ 70 km高度降水过程中N2(X1 ~ g+, v′= 1)浓度和臭氧O3和氧化亚氮N2O红外波段的发射强度。结果表明,在给定的相对论电子通量为105 e/cm2·s·ster的情况下,在50 ~ 70 km的中层大气高度,振动激发的分子氮N2(X1′g+, v′= 1)的浓度约为105 ~ 106 cm-3。计算了臭氧在4.7µm和9,9µm的红外波段以及氧化亚氮在4.5µm的红外波段的发射谱线,得到了能量为E = 2,4,10 MeV的高能电子的析出。首次证明了在高能电子的沉淀过程中,振动激发的氮气N2(X1′g+, v′= 1)与O3和N2O分子发生非弹性碰撞,在改变中层大气红外平衡中起着重要作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The influence of vibrationally excited molecular nitrogen on infrared emissions of O3 and N2O gases at altitudes of the middle atmosphere
The concentrations of N2(X1g+, v' = 1) and the emission intensities of infrared bands of ozone O3 and nitrous oxide N2O are calculated at altitudes of 30–70 km of the Earth's middle atmosphere during precipitation of electrons with energies E = 2, 4, 10 MeV. It is shown that for a given relativistic electron flux of 105 e/cm2·s·ster, the concentrations of vibrationally excited molecular nitrogen N2(X1g+, v' = 1) are about 105–106 cm–3 at altitudes of 50–70 km of the middle atmosphere. The emission profiles of the infrared bands of ozone at 4.7 µm and 9,9 µm, as well as the infrared band of nitrous oxide at 4.5 µm, are calculated for precipitation of high-energy electrons with energies E = 2, 4, 10 MeV. It has been shown for the first time that vibrationally excited nitrogen N2(X1g+, v' = 1) plays an important role in changing the infrared balance of the middle atmosphere as a result of inelastic molecular collisions with O3 and N2O molecules during precipitation of high-energy electrons.
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