Investigation of variations of the vertical temperature profile on the basis of experimental observations of cosmic-ray intensity

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Atmospheric Temperature, Cosmic Rays, Muons, Particle Flux Density, Temperature Profiles, Vertical Distribution, Heat Transfer Coefficients, Temperature Measuring Instruments, Temporal Distribution

Scientific paper

An effort is made to demonstrate that the time variations of the vertical temperature profile of the earth's atmosphere can be determined by measuring the intensity of the muon component of cosmic rays. The method used to establish this relationship is Dorman's (1957) approach involving the application of temperature-coefficient densities. A neutron-monitor system for measuring the vertical temperature profile in the manner proposed is described.

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