Seasonal and diurnal variations in the ionic content of the Earth’s average atmosphere and ionosphere

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Abstract

The high-latitude atmosphere is ionized by direct solar radiation. This leads to the formation of positively charged ions through, for example, photo-adhesion and ionization of NO. In this work, using a one-dimensional chemical and climatic model with interactive neutral and ionic chemistry, we tracked the ionic compositions of the D region of the ionosphere on daily and seasonal scales.

About the authors

D. V Grankin

Saint-Petersburg State University

Saint-Petersburg, Russia

I. A Mironova

Saint-Petersburg State University

Email: i.a.mironova@spbu.ru
Saint-Petersburg, Russia

E. V Rozanov

Saint-Petersburg State University

Saint-Petersburg, Russia

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