Abstract. On the basis of field and particle observations, it is suggested that a bright auroral display is a part of a magnetosphere-ionosphere current system which is fed by a charge-separation process in the outer magnetosphere (or the solar wind). The upward magnetic-field-aligned current is flowing out of the display, carried mainly by downflowing electrons from the hot-particle populations in the outer mag netosphere (the ambient cold electrons being depleted at high altitudes). As a result of the magnetic mirroring of these downflowing current carriers, a large potential drop is set up along the magnetic field, increasing both the number flux and the kinetic energy of precipitating electrons. It is found that this simple basic model, when combined with wave-particle interactions, may be able to explain a highly diversified selection of auroral particle observations. It may thus be possible to explain both "inverted-V" events and auroral rays in terms of a static parallel electric field, and the electric field may be compatible with a strongly variable pitch-angle distribution of the precipitating electrons, including distributions peaked at 900 as well as 00. This model may also provide a simple explanation of the simultaneous precipitation of electrons and collimated positive ions.
IntroductionOne of the most puzzling problems in magnetospheric physics today is how to understand the complex processes that cause energization and precipitation of the auroral For reference purposes we need a rough division of current ideas about auroral particle acceleration. The main ideas may be grouped into the following three basic categories:(a) The precipitating particles have already attained their final energy when leaving the equatorial region of the magnetosphere. It is frequently assumed that the auroral particles get their final energy by, for instance, betatron and Fermi acceleration during their drift motion into and filling of the plasma sheet reservoir with energetic particles. In order for a sufficient flux of the energized particles to reach down to the atmosphere, despite the strong mirroring effect of the geomagnetic field, a final pitch-angle scattering mechanism (by means of wave-particle inter actions) may be needed. See, for instance, Kennel and Petschek (1966). Some measurements of the near earth plasma sheet seem to indicate a sufficient energy flux of particles with appropriate energies for producing even the most intense auroral precipi tation (Frank, 1971;Vasyliunas, 1970). For a very brief review of this kind of large scale energization, see Heikkila (1974).(b) The precipitating particles in general, or at least some of them, gain additional energy at the expense of a trapped particle component through which they pass on their way down. Alternatively, this energy transfer may be from one precipitating component to the other. According to this view the energy yielding particles having an unstable velocity distribution produce plasma waves, the energy of which is absorbed by the precipitating par...