Cosmic ray north-south anisotropy: The role of the interplanetary magnetic field
- 1. Bartol Research Foundation of the Franklin Institute University of Delaware, Newark, Delaware 19711
Description
Nucleonic intensity data from the north and south polar stations Thule and McMurdo are analyzed to determine the nature of periodicities in the north-south asymmetry of relativistic galactic cosmic rays. The 24-hour average intensity differences of individual days range from 0 to +- 1.5%, and the most prominent time variation is recurrence tendency with a period consistent with the 27-day solar rotation period. A recently developed procedure for evaluating the statistical significance of quasipersistent data has been utilized to establish the reality of the 27-day signal disclosed by superposed epoch analysis of the north-south asymmetry data. Analyses of various components of the interplanetary magnetic field reveal that the IMF component B-bar/sub μ/ (parallel to the nominal garden hose direction) also displays a 27-day variation with maximum amplitude. Furthermore, a significant relationship between B-bar/sub μ/ and the north-south asymmetry is established by Chree analysis. On the basis of this relationship, it is suggested that the 27-day variation in the north-south asymmetry arises from the B-bar/sub μ/ x del-bar(n) drift, where del-bar(n) represents the radial gradient of cosmic rays
Additional details
Publishing Information
- Journal Title
- J. Geophys. Res.
- Journal Volume
- 87
- Journal Issue
- A12
- Series
- J. Geophys. Res.
- Journal Page Range
- 10325-10330
- ISSN
- 0022-1406
INIS
- Country of Publication
- United States
- Country of Input or Organization
- United States
- INIS RN
- 14785223
- Subject category
- S79: ASTROPHYSICS, COSMOLOGY AND ASTRONOMY;
- Descriptors DEI
- FREQUENCY DEPENDENCE; INTERPLANETARY MAGNETIC FIELDS; NORTH-SOUTH ASYMMETRY; PRIMARY COSMIC RADIATION; STATISTICS; VARIATIONS
- Descriptors DEC
- ASYMMETRY; COSMIC RADIATION; IONIZING RADIATIONS; MAGNETIC FIELDS; MATHEMATICS; RADIATIONS