Author:
Nagashima K.,Ueno H.,Mori S.,Sagisaka S.
Abstract
The sidereal time variation is analyzed using data for the ion chambers at Cheltenham and Christchurch for the period 1938–58 and for the meson and neutron components during the IGY. All the results derived from these three kinds of data support the existence of a two-way sidereal anisotropy, suggested by Jacklyn, which has two maxima of the cosmic-ray intensity in the directions of 8 h and 20 h S.T. (sidereal time).
Publisher
Canadian Science Publishing
Subject
General Physics and Astronomy
Cited by
6 articles.
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