Geomagnetism and Aeronomy

, Volume 48, Issue 3, pp 327–336

Anomalous variations in the ionospheric F 2-layer structure at geomagnetic midlatitudes of the Southern and Northern hemispheres at the transition from summer to winter conditions under low solar activity

Authors

    • Institute of Terrestrial Magnetism, Ionosphere, and Radiowave PropagationRussian Academy of Sciences
  • N. M. Pavlova
    • Institute of Terrestrial Magnetism, Ionosphere, and Radiowave PropagationRussian Academy of Sciences
  • S. F. Makarenko
    • Institute of Terrestrial Magnetism, Ionosphere, and Radiowave PropagationRussian Academy of Sciences
  • V. N. Shubin
    • Institute of Terrestrial Magnetism, Ionosphere, and Radiowave PropagationRussian Academy of Sciences
Article

DOI: 10.1134/S0016793208030080

Cite this article as:
Pavlov, A.V., Pavlova, N.M., Makarenko, S.F. et al. Geomagn. Aeron. (2008) 48: 327. doi:10.1134/S0016793208030080

Abstract

The structure and dynamics of the ionosphere and plasmasphere at low solar activity under quiet geomagnetic conditions on January 15–17, 1985, and July 10–13, 1986, over Millstone Hill station and Argentine Islands ionosonde, the locations of which are approximately magnetically conjugate, have been theoretically calculated. The detected correction of the model input parameters makes it possible to coordinate the measured and calculated anomalous variations in the electron density NmF2 at the height hmF2 of the ionospheric F2 layer over Argentine Islands ionosonde as well as the calculated and measured values of NmF2 and electron temperature at the hmF2 height over Millstone Hill station. It has been shown that vibrationally excited N2 and O2 molecules almost do not influence the formation of the winter anomaly under the conditions of low solar activity. A difference between the influence of electronically excited O+ on N e ions under winter and summer conditions forms not more than 11% of the N e winter anomaly event in the F 2 layer and topside ionosphere. The model without electronically excited O+ ions reduces the duration of the N e winter anomaly event. It has been shown that the seasonal variations in the composition of the neutral atmosphere form mainly the NmF2 winter anomaly event over the Millstone Hill radar at low solar activity.

PACS numbers

94.20.Dj 96.60.Qd

Copyright information

© Pleiades Publishing, Ltd. 2008