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AGU: Journal of Geophysical Research, Space Physics

 

Index Terms

  • Atmospheric Composition and Structure: Thermosphere—composition and chemistry
  • Atmospheric Composition and Structure: Thermosphere—energy deposition
  • Atmospheric Composition and Structure: Airglow and aurora
  • Magnetospheric Physics: Auroral phenomena
Abstract
Cited By (41)
 

Abstract

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, 1027, 11 PP., 2003
doi:10.1029/2002JA009458

Global observations of nitric oxide in the thermosphere

C. A. Barth

Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, Colorado, USA

K. D. Mankoff

Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, Colorado, USA

S. M. Bailey

Geophysical Institute, University of Alaska, Fairbanks, Alaska, USA

S. C. Solomon

High Altitude Observatory, National Center for Atmospheric Research, Boulder, Colorado, USA

Nitric oxide density in the lower thermosphere (97–150 km) has been measured from the polar-orbiting Student Nitric Oxide Explorer (SNOE) satellite as a function of latitude, longitude, and altitude for the 2 1/2 year period from 11 March 1998 until 30 September 2000. The observations show that the maximum density occurs near 106–110 km and that the density is highly variable. The nitric oxide density at low latitudes correlates well with the solar soft X-ray irradiance (2–7 nm), indicating that it is the solar X-rays that produce thermospheric nitric oxide at low and midlatitudes. Nitric oxide is produced at auroral latitudes (60°–70° geomagnetic) by the precipitation of electrons (1–10 keV) into the thermosphere. During high geomagnetic activity, increased nitric oxide may be present at midlatitudes as the result of meridional winds that carry the nitric oxide equatorward.

Published 18 January 2003.

Citation: Barth, C. A., K. D. Mankoff, S. M. Bailey, and S. C. Solomon (2003), Global observations of nitric oxide in the thermosphere, J. Geophys. Res., 108(A1), 1027, doi:10.1029/2002JA009458.

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