Observations of N2 in the Lower Thermosphere by the RAIDS Experiment

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[0355] Atmospheric Composition And Structure / Thermosphere: Composition And Chemistry

Scientific paper

Utilizing the RAIDS Extreme Ultraviolet Spectrograph (EUVS) on the ISS we present measurements of thermospheric N2 in the altitude range of 100-300km. One of the dominant features present in the EUVS observing wavelength range 770 - 1100 Å is N II (1085 Å). N2 emissions in the atmosphere primarily results from hν + N2 → N2+(H + H’) → 1085 Å [Meier et al., 1991] with significant contributions to the emission below 150 km by e- + N2 [Bishop and Feldman, 2003]. Previous experiments have noted that the N2 emission rapidly increases between ~130 to ~200 km where it reaches a nearly constant emission intensity [Bishop and Feldman, 2003]. Other results from the Air Force STP 78-1 satellite showed an increase in N2 intensities between + 20 latitude during [Chakarabarti et al., 1983]. This talk presents observations of N2 observed by the RAIDS instrument throughout the last year. We show the variability as a function of altitude, and latitude/longitude and compare the results with earlier observations. Additionally, by determining the scale height of N2 we will calculate an exospheric temperature profile up 300 km. References: Bishop, J., P. D. Feldman, Analysis of the Astro-1/Hopkins Ultraviolet Telescop EUV-FUV dayside nadir spectral radiance measurements, J. Geophys. Res., 108(A6), doi:10.1029/2001JA000330, 2003. Chakrabarti, S., F. Paresce, S. Bowyer, R. Kimble, The Extreme Ultraviolet Day Airglow, J. Geophys. Res., 88(A6), 4898-4904, 1983. Meier, R. R., J. A. R. Samson, Y. Chung, E.-M. Lee, and Z.-X. He, Production of N+* from N2+ hv: Effective EUV emission yields from laboratory and dayglow data, Planet. Space Sci., 39, 1197-1207, 1991.

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