Study of the Earth’s Own Radiation of the Upper Atmosphere (Herzberg I Bands) as a Function of Solar Activity, Atmospheric Temperature, and Seasons of the Year

Author:

Antonenko O. V.,Kirillov A. S.

Publisher

Pleiades Publishing Ltd

Subject

Atmospheric Science,Oceanography

Reference14 articles.

1. N. N. Shefov, A. I. Semenov, and V. Yu. Khomich, Radiation of the Upper Atmosphere as an Indicator of its Structure and Dynamics (GEOS, Moscow, 2006) [in Russian].

2. A. L. Broadfoot and P. J. Bellaire, Jr., “Bridging the gap between ground-based and space-based observations of the night airglow,” J. Geophys. Res. 104 (A8), 17127–17138 (1999).

3. V. I. Perminov, A. I. Semenov, and N. N. Shefov, “Deactivation of hydroxyl molecule vibrational states by atomic and molecular oxygen in the mesopause region,” Geomagn. Aeron. (Engl. Transl.) 38 (6), 761–764 (1998).

4. A. I. Semenov and N. N. Shefov, “Variations in the temperature and atomic-oxygen concentration of the mesopause–lower thermosphere region according to variations in solar activity,” Geomagn. Aeron. (Engl. Transl.) 39 (4), 484–487 (1999).

5. A. I. Semenov and N. N. Shefov, “An empirical model of nocturnal variations in the 557.7-nm emission of atomic oxygen: 1. Intensity,” Geomagn. Aeron. (Engl. Transl.) 37 (2), 215–221 (1997).

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