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The vibrational distribution of N 2 + in the terrestrial ionosphere

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1985-08-01

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American Geophysical Union (AGU)
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Fox, J. L., and A. Dalgarno. 1985. “The Vibrational Distribution of N 2 + in the Terrestrial Ionosphere.” Journal of Geophysical Research: Space Physics 90 (A8) (August 1): 7557–7567. doi:10.1029/ja090ia08p07557.

Abstract

The densities and vibrational distributions of N2+ in the X²Σg+, A²Πu, and B²Σu+ states in the daytime terrestrial ionosphere are computed for both low and high solar activity. Altitude profiles of the relative populations of the vibrational levels of N2+X²Σg+ are presented. The fraction of vibrationally excited N2+ varies from 5% at 100 km to 50% at 450 km. Several models are examined in which loss of N2+(v) is enhanced for v > 0 and in which various assumptions are made about the vibrational distributions produced in charge transfer reactions. The N2+ densities are significantly reduced if N2+(v) reacts with O at rates which are near gas-kinetic. Vibrational distributions of the A²Πu and B²Σu+ states are also presented, as well as volume emission rates and integrated overhead intensities of the major bands of the Meinel and first negative systems.

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Paleontology, Space and Planetary Science, Earth and Planetary Sciences (miscellaneous), Atmospheric Science, Earth-Surface Processes, Geochemistry and Petrology, Soil Science, Water Science and Technology, Ecology, Aquatic Science, Forestry, Oceanography, Geophysics

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