2006
DOI: 10.1029/2005ja011348
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Measurements of rovibronic line oscillator strengths of N2 in the 83.4 nm region: A high‐resolution high‐temperature study

Abstract: [1] We report the rovibronic line oscillator strengths of N 2 in the 83.4 nm region at high temperatures measured by using ultrahigh-resolution photoabsorption spectroscopy. The measurements have been carried out using a resolution of 6.5 Â 10 À4 nm and at temperatures of 600, 535, and 295 K. The N 2 absorption features in the 83.4 nm region mainly involve the (0,0) band of the c

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Cited by 2 publications
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“…Though the majority of the 83.4 nm emission from Earth's airglow in the lower ionosphere originates from solar EUV photoionization‐excitation of atomic oxygen, with some from electron impact [ Link et al , 1994], complete analysis of auroral emissions (at lower altitudes) should involve some e − + O 2 contribution [ LeClair and McConkey , 1993; Zipf et al , 1985a]. Modeling of the 83.4 nm emission region is complicated by temperature‐dependent photoabsorption by N 2 and O 2 , which can skew the overlapped O II (83.4 nm) multiplet emissions via the changing ro‐vibrational contributions from N 2 [ Wu et al , 2006]. Also, proton‐stimulated auroral emissions involve a secondary electron component, which is less energetic than from electron‐based auroras and thus have different spectral characteristics [ Galand and Lummerzheim , 2004; Simon et al , 2007].…”
Section: Introductionmentioning
confidence: 99%
“…Though the majority of the 83.4 nm emission from Earth's airglow in the lower ionosphere originates from solar EUV photoionization‐excitation of atomic oxygen, with some from electron impact [ Link et al , 1994], complete analysis of auroral emissions (at lower altitudes) should involve some e − + O 2 contribution [ LeClair and McConkey , 1993; Zipf et al , 1985a]. Modeling of the 83.4 nm emission region is complicated by temperature‐dependent photoabsorption by N 2 and O 2 , which can skew the overlapped O II (83.4 nm) multiplet emissions via the changing ro‐vibrational contributions from N 2 [ Wu et al , 2006]. Also, proton‐stimulated auroral emissions involve a secondary electron component, which is less energetic than from electron‐based auroras and thus have different spectral characteristics [ Galand and Lummerzheim , 2004; Simon et al , 2007].…”
Section: Introductionmentioning
confidence: 99%