Seasonal and diurnal variations of cosmic-ray intensity according to measurement at a depth of about 8.5 x 10 to the 4th g/sq cm

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Annual Variations, Cosmic Rays, Earth Atmosphere, Radiant Flux Density, Atmospheric Boundary Layer, Atmospheric Temperature, Upper Atmosphere

Scientific paper

Baksan scintillation-counter measurements for a period extending from
January 1, 1983 to December 31, 1987 are analyzed. It is shown that
seasonal variations of the intensity of the cosmic-ray muon component at
energies not less than 220 GeV are caused by thermal processes in the
upper layers of the atmosphere.

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