Relationship between the amplitude and phase of cosmic-ray anisotropy near two minima of solar activity

Computer Science

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Convection-Diffusion Equation, Cosmic Rays, Diurnal Variations, Interplanetary Medium, Solar Activity Effects, Amplitude Distribution Analysis, Anisotropy, Phase Deviation

Scientific paper

An analysis of diurnal values of cosmic-ray (CR) anisotropy components obtained from the global network of neutron monitors for the 1970s and 1980s shows a specific relationship between the amplitude and phase of the solar-diurnal variation. This relationship and differences in the anisotropy for two different solar minima are explained by the convective-diffusive model of anisotropy, taking into account all three components of the CR gradient. Distributions of the radial and latitudinal CR gradients in the solar wind in the vicinity of the earth are calculated for the 1974-1977 and 1984-1987 periods.

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