A Scintillation Hodoscope for Investigating the Muonic Component of Cosmic Rays at the Tien Shan Mountain Station

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A Scintillation Hodoscope for Investigating the Muonic Component of Cosmic Rays at the Tien Shan Mountain Station

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The data of measurements taken near Elbrus in the (600÷1000) mb atmospheric-depth range are used to study the angular distribution and the altitude dependence of the cosmic-ray general and muon components. The measurements were taken with a system of scintillation telescopes at 0°, 30°, 45° and 60° zenith angles and at 100°, 80°, 65° and 40° apertures, respectively. The muon component was isolated with a 10 cm thick lead screen. The angular distribution was set in the formI(θ,h)=I0(h)[cos θ]n(h), where θ is the zenith angle,h is the atmospheric depth. Relations have been obtained which permit the parametern(h) to be plotted on the basis of the measured values of cosmic-ray intensity at various depths by using the above-mentioned four telescopes. It has been found that, ash varies from 600 to 1000 mb,n varies from 0.6 to 1.6 for the muon component and from 1.2 to 1.9 for the general component. The found altitude dependences permit the barometric coefficients to be determined for the various detection directions as functions of the pressure at the observation level.

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Correction of meteorological effects on muon component of secondary cosmic rays significantly extends the usability of muon monitors. We propose a new data driven empirical method for correction of meteorological effects on muon component of secondary cosmic rays, based on multivariate analysis. Several multivariate algorithms implemented in Toolkit for Multivariate Data Analysis with ROOT framework are trained and then applied to correct muon count rate for barometric and temperature effects. The effect of corrections on periodic and aperiodic cosmic ray variations is analyzed and compared with integral correction method, as well as with neutron monitor data. The best results are achieved by the application of linear discriminant method, which increases sensitivity of our muon detector to cosmic ray variations beyond other commonly used methods.

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A time-independent linear stability analysis is performed on a self-gravitating, plane-parallel, isothermal layer of nonrotating gas with magnetic and cosmic-ray components. The gas layer is immersed in a rigid plane-stratified isothermal layer of stars which supply a self-consistent gravitational field. The stability analysis is confined to disturbances which propagate along the magnetic field. The principal result to emerge from this study is that the magnetic field and cosmic-ray gas hinder gravitational instability, increasing the minimum length necessary to produce instability approximately by the factor (1 + a + )112, where a is the ratio of magnetic pressure to gas pressure and P is the ratio of cosmic-ray pressure to gas pressure. The author has recently shown that a similar result applies when disturbances propagate across the magnetic field. Subject headings: cosmic rays - hydromagnetics - instabilities

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