It has long been known that the physical state of the Earth’s upper atmosphere is closely related to solar activity-the growth and decay of sunspots, the corona, uprushing prominences and bright chromospheric flares. In particular, transient radiative and corpuscular emissions associated with solar flares produce the most outstanding electromagnetic disturbances in the environment of the Earth. It is generally believed that geomagnetic storms are caused by the impact of solar plasma clouds with the geomagnetic field(l). Associated aurora1 and ionospheric effects are the direct consequence of disturbances induced in the upper atmosphere. The evidence of continual agitation of the geomagnetic field in the polar regions suggests a constant stream of incoming particles even during geomagnetically quiet periods. This accords with certain observations of the motion of comet tailP, for which the name solar wind or streaming plasma has been proposed in contrast to the storm-producing plasma cloud(3). The accumulated evidence of recent years indicates that the Sun emits not only lowenergy plasmas but also, on occasions, very-high-energy particles, known as solar cosmic raysc4). Since 1942, eight events showing an unusual increase in cosmic ray intensity have been found in ground-based observations. They were associated with intense solar flares, and the particles arrived at the Earth within very short time-delay, indicating that the energy exceeded the relativistic range. Several small but distinct solar cosmic ray events have also been identified since the International Geophysical Year (1957-8) strengthened considerably the precise world network of neutron monitors. An arrival of sub-relativistic-energy particles is not detectable at ground level, but this information is now available from recently developed rocket and balloon measurements and indirectly by ionospheric observations. These particles emitted from a solar flare impinge onto the ionosphere in the polar-cap regions, thereby producing enhanced ionization and a particular type of aurora1 glow. Thus, the events are known as polar-cap blackouts(5-7), polar-cap absorptionPlO) and polar-glow auroraeol). Direct measurements by balloon(12) and by satellites (13) .have revealed that the energy spectrum of these solar particles is considerably broad, ranging from 1 to 1000 MeV. Statistical studies have shown that such events are much more numerous than was ever suspectedo4), and also that they are closely related to the particular type of solar flares associated with strong radio outbursts of continuum radiationul in particular, comprehensive measurements by recent space probes and satellites. Thus, it is now evident that an enormous number of particles with a considerable wide-energy spectrum is streaming out from the Sun. Since solar particles detected in the environment of