Cosmic ray research began in 1912 when Victor Hess measured the intensity of the then unknown ionizing radiation with an electroscope in a balloon up to an altitude of about 5,000 m. He discovered that this very penetrating radiation, later called cosmic rays, was coming from outside the atmosphere (for a historic review, see Simpson, 2001).The systematic experimental study of cosmic rays began in the 1930s, using ground-based and balloon-borne ionization chambers. In the 1950s it expanded on a much larger scale with neutron monitors, coordinated world-wide during the International Geophysical Year (IGY) in 1957 (Simpson, 2000). When Parker (1958) described the solar wind, the theoretical research of cosmic rays began, stimulated by the beginning of in situ space observations that have led over four decades to important space missions, including the Ulysses mission to high heliolatitudes.
Particle populations in the heliosphereWithin the heliosphere, energetic charged particles of different origin can be identified. In the previous chapters solar energetic particles and particles accelerated by interplanetary shock waves have been discussed. In what follows we will only discuss galactic and anomalous cosmic rays, Jovian electrons, and their propagation and modulation in the heliosphere.
Galactic cosmic raysGalactic cosmic rays (GCRs) consist of energetic electrons and nuclei which are a direct sample of material from far beyond the solar system. They are accelerated by shock waves in the galaxy from, for example, supernova remnants, pulsars, or active galactic nuclei. The remarkable feature of cosmic rays is their energy spectra,