Modelling the Cosmic Ray (CR) Effect in the Polar Ionosphere with Account of Anomalous CR-Component

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Cosmic Rays, Anomalies, Earth Ionosphere, Polar Regions, D Region, Radio Waves, Middle Atmosphere, Latitude, Pascal (Programming Language), Atmospheric Ionization

Scientific paper

The lower part of the D-region is created by cosmic rays which form there an independent Cosmic Ray (CR)-layer. The CR-layer is important for the propagation of the long and very long radio waves. For that reason the rates investigation of the ionization rates in the middle atmosphere is significant for the understanding of the electric and other physical and chemical processes there. The CR-layer is a boundary layer between the ionosphere and the neutral gas in the stratosphere. Actually a few models for cosmic ray influence on the middle latitude ionosphere exist. But the effects of the high energy cosmic particles are much more essential in the polar ionosphere, because of the comparatively weak geomagnetic cut-offs. For that reason in the present paper a more adequate model of high latitude ionization of cosmic rays is proposed. The model will include the recently discovered anomalous component of cosmic rays.

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