Geocoronal hydrogen observations spanning three solar minima

Type Journal Article
Names S. M. Nossal, E. J. Mierkiewicz, F. L. Roesler, L. M. Haffner, R. J. Reynolds, R. C. Woodward
Publication Journal of Geophysical Research (Space Physics)
Volume 113
Issue A11
Pages 11307
Date November 1, 2008
URL http://adsabs.harvard.edu/abs/2008JGRA..11311307N
Library Catalog NASA ADS
Abstract The 11-year solar cycle is a dominant source of natural variability in the upper atmosphere, and its effect on atomic hydrogen distributions and emissions must be understood to investigate possible signs of longer-term climatic trends in this region. We present midlatitude geocoronal hydrogen Balmer α observations from solar cycle 23 (1997-2006) and three solar minimum periods, 1985, 1997, and 2006. The 1997 through 2006 observations were taken with the Wisconsin H-α Mapper Fabry-Perot (WHAM), a ground-based CCD-annular summing instrument that began observations at the Kitt Peak Observatory in Arizona in 1997. The 1985 observations were made with a similarly designed ``pre-WHAM'' Fabry-Perot Interferometer utilizing photomultiplier detection and located in Wisconsin. WHAM has consistently observed higher column emission intensities during solar maximum periods than during solar minimum conditions, with the ratio dependent upon the viewing geometry. The observations from three solar minimum periods agree to within 18% uncertainties over most of the shadow altitude range. An analysis of recent Fabry-Perot observations of upper atmospheric hydrogen during solar cycle 23 and during three solar minima (1985, 1997, 2006) established a reference data set of highly precise, consistently calibrated, thermospheric plus exospheric hydrogen column emission observations from northern midlatitudes that can be used to compare with future observations.
Tags 1635, 3309, 4215, 4513), Atmospheric Composition and Structure: Airglow and aurora, Atmospheric Composition and Structure: Exosphere, Atmospheric Composition and Structure: Thermosphere: composition and chemistry, Atmospheric Processes: Climate chang
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