Ionic mobility of the middle atmosphere

Positive ion mobilities are calculated for 40–75 km by computing the theoretical positive ion composition and combining it with laboratory-determined mobilities. Theoretical determinations for mobility appear to be especially apt for the 40–65 km region since oxonium ions are observed to be the prin...

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Veröffentlicht in:	Advances in space research 1984, Vol.4 (6), p.29-32
1. Verfasser:	Swider, William
Format:	Artikel
Sprache:	eng
Online-Zugang:	Volltext
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