Atomic nitrogen measurements in the upper thermosphereThe open source neutral mass spectrometer on board the Atmosphere Explorer satellites measures, besides other neutral constituents, atomic nitrogen densities in the upper thermosphere. Atomic nitrogen combines with atomic oxygen on the walls of the mass spectrometer ion source to form NO. From the measured NO concentration atomic nitrogen is deduced. Studies of the diurnal variation show that the maximum atomic nitrogen densities occur near 1600 local solar time (LST) and minimum densities near 0400 LST. The diurnal amplitude at 300 km is about a factor of 8, which is lower than predicted in present models. Atomic nitrogen also exhibits a pronounced seasonal variation with an amplitude similar to that of the diurnal variation; summer values are considerably higher than winter ones.
Document ID
19780034225
Acquisition Source
Legacy CDMS
Document Type
Conference Proceedings
Authors
Mauersberger, K. (Minnesota Univ. Minneapolis, MN, United States)
Engebretson, M. J. (Minnesota Univ. Minneapolis, MN, United States)
Potter, W. E. (Minnesota Univ. Minneapolis, MN, United States)
Kayser, D. C. (Minnesota Univ. Minneapolis, MN, United States)
Nier, A. O. (Minnesota, University Minneapolis, Minn., United States)
Date Acquired
August 9, 2013
Publication Date
January 1, 1977
Subject Category
Geophysics
Meeting Information
Meeting: Symposium on Minor Constituents and Excited Species