Magnetospheric processes and related geophysical phenomena

In this paper we consider those processes mainly related to the behaviour of the low-energetic magnetospheric plasma, which nevertheless contains the main mass and the predominant part of the thermal energy. Our attention has been concentrated on those processes which, from our point of view, determine geomagnetic phenomena on the surface of the earth. Because of the scope of the project, we had to exclude the processes of acceleration of high-energetic particles in the tail of the magnetosphere, their diffusion deep within, and the formation of the radiation belts. These problems are of independent interest and may be considered separately.When describing various phenomena we tried to stress the principal side of a question without regard to the details of one theory or other, though we did not keep to this principle throughout. Together with the results which are dealt with in the literature, we took the risk of including those considerations which are not as yet published. It mainly concerns Sections 2.3, 2.4, 3.4, 3.6, 3.7, and 4. where, together with other problems, three new hypotheses of the main phase of a storm and of Sq-variations are discussed. We prefer the mechanism connected with the current induction in the ionosphere (Section 4.4). For this purpose some aspects of magnetohydrodynamics were examined (Section 4.3).