O/N2 changes during 1–4 October 2002 storms: IMAGE SI‐13 and TIMED/GUVI observations

By Yongliang Zhang, Larry J. Paxton, D. Morrison, B. Wolven, H. Kil, C. Meng, S. Mende, T. Immel. 2004

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Ionospheric response to the 2015 St. Patrick's Day storm: A global multi‐instrumental overview (2015, background): “These comprise composition changes [e.g., Zhang et al., 2004; Crowley et al., 2006], penetration of electric fields [e.g., Huang et al., 2005], disturbance dynamo electric fields [Blanc and Richmond, 1980], thermospheric winds [e.g., Balan et al., 2011], or a combination of those.”
Seasonal variation of thermospheric density and composition (2009, methodology): “6 nm) andN2 LBHmolecular bands (141 to 153 nm), are used to derive column number density ratio O/N2 above an altitude where the N2 column density is 10 17 cm 2 (approximately 140 km) [Strickland et al., 2004; Zhang et al., 2004].”