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The role of nitric oxide on the zonally averaged structure of the thermosphere: Solstice conditions for solar cycle minimum

  • Published:1986-02 Issue:2 Volume:34 Page:131-144
  • ISSN:0032-0633
  • Container-title:Planetary and Space Science
  • language:en
  • Short-container-title:Planetary and Space Science

Author:

Gërard J.Cl.,Roble R.G.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Astronomy and Astrophysics

Reference44 articles.

1. The temperature of the upper atmosphere;Bates,1951

2. Global morphology of nitric oxide in the lower E-region;Cravens;J. geophys. Res.,1978

3. The latitudinal gradient of nitric oxide in the lower thermosphere;Cravens;J. geophys. Res.,1979

4. The global distribution of thermospheric nitric oxide as observed by the Atmosphere Explorer D satellite;Cravens;J. geophys. Res.,1986

5. Method of parameterization for infrared cooling between altitudes of 30 and 70 kilometers;Dickinson;J. geophys. Res.,1973

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