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Reversal of the cosmic ray density gradient perpendicular to the ecliptic plane

Journal Article · · J. Geophys. Res.; (United States)
Annual averages of the diurnal variation in cosmic ray intensity from neutron monitors in Deep River and Oulu and underground muon telescopes in Bolivia and at Embudo and Socorro, New Mexico, have been determined as a function of the sense of the interplantary magnetic field for the years 1965--1975. These data point to a cosmic ray density gradient, perpendicular to the ecliptic plane, pointing southward prior to 1969 and changing to a northward pointing gradient after the reversal of the sun's polar magnetic field in 1969--1971. This result supports numerical calculations for the prereversal and postreversal field configurations at intermediate and high cosmic ray rigidities.
Research Organization:
Department of Physics and Astronomy, University of New Mexico, Albuquerque, New Mexico 87131
OSTI ID:
6864647
Journal Information:
J. Geophys. Res.; (United States), Journal Name: J. Geophys. Res.; (United States) Vol. 87:A3; ISSN JGREA
Country of Publication:
United States
Language:
English