Answers are grounded in this paper and cite their sources.
Extreme ultraviolet auroral spectra have been obtained in the wavelength range of 750‐1230 A resolution with a rocket‐borne grating spectrometer. Atomic emissions of NI, NII, OI and OII are the dominant features along with geocoronal HI Lyman α. N 2 emission bands, which appear strongly in laboratory electron impact spectra, appear only as a modest background continuum between 900 to 1100 A. The observed intensities are consistent with electron impact excitation of O and N 2 . For optically thick emissions, such as NI λ1200, radiation transport along the arc results in an intensity enhancement when viewed through the arc towards the zenith.
No takes yet. Share an insight, caveat, or question.
Park et al. (1977) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: