The large amplitude wave-trains of cosmic-ray intensity observed during June, July and August, 1973, were analysed. These events exhibit the same characteristics as the event of May, 1973. During these days the phase of the enhanced diurnal anisotropy is shifted to a point earlier than either the corotation direction or the anti-garden-hose direction. For this analysis we used data from high- and middle-latitude neutron monitors and from the satellites HEOS-2, IMP-7 and IMP-8. The diurnal variation of these days is well understood in terms of a radially outward convective vector and a field-aligned inward diffusive vector yielding a diurnal anisotropy vector along about 1600 h in space. © 1980 D. Reidel Publishing Co
The results of a measurement of the anisotropic character of the cosmic radiation in the vicinity of...
Abstract: The cosmic ray (CR) intensity data recorded with Deep River Neutron Monitoring Station hav...
A study of cosmic ray intensity variations has been conducted during 1956–57 at the equatorial mount...
Using ground-based neutron monitor data of Deep River, the high amplitude anisotropic wave train eve...
232-235The high amplitude anisotropic wave train events (HAEs) in cosmic ray (CR) intensity have bee...
In this paper an attempt is made to study the occurrence of a large number of high amplitude anisotr...
A detailed study has been conducted on the long-term changes in the diurnal, semi-diurnal and tri-di...
9-13In the present study the occurrence of a large number high amplitude event (HAE) of cosmic ray d...
The diurnal anisotropy of cosmic ray intensity has been investigated over the interval 1973\u2013197...
312-318A large number of low amplitude anisotropic wave train events (LAEs) of cosmic ray diurnal an...
189-196 Cosmic ray (CR) intensity shows significant diurnal variations of day-to-day most probable a...
The occurrence of a large number high amplitude event (HAE) of cosmic ray diurnal anisotropy during ...
The diurnal anisotropy of cosmic ray intensity for the time period 2001 to 2014 is studied, coverin...
From an analysis of the data from the worldwide network of neutron monitor stations, the general cha...
233-236The average behaviour of the daily variation of cosmic ray intensity has been studied for a l...
The results of a measurement of the anisotropic character of the cosmic radiation in the vicinity of...
Abstract: The cosmic ray (CR) intensity data recorded with Deep River Neutron Monitoring Station hav...
A study of cosmic ray intensity variations has been conducted during 1956–57 at the equatorial mount...
Using ground-based neutron monitor data of Deep River, the high amplitude anisotropic wave train eve...
232-235The high amplitude anisotropic wave train events (HAEs) in cosmic ray (CR) intensity have bee...
In this paper an attempt is made to study the occurrence of a large number of high amplitude anisotr...
A detailed study has been conducted on the long-term changes in the diurnal, semi-diurnal and tri-di...
9-13In the present study the occurrence of a large number high amplitude event (HAE) of cosmic ray d...
The diurnal anisotropy of cosmic ray intensity has been investigated over the interval 1973\u2013197...
312-318A large number of low amplitude anisotropic wave train events (LAEs) of cosmic ray diurnal an...
189-196 Cosmic ray (CR) intensity shows significant diurnal variations of day-to-day most probable a...
The occurrence of a large number high amplitude event (HAE) of cosmic ray diurnal anisotropy during ...
The diurnal anisotropy of cosmic ray intensity for the time period 2001 to 2014 is studied, coverin...
From an analysis of the data from the worldwide network of neutron monitor stations, the general cha...
233-236The average behaviour of the daily variation of cosmic ray intensity has been studied for a l...
The results of a measurement of the anisotropic character of the cosmic radiation in the vicinity of...
Abstract: The cosmic ray (CR) intensity data recorded with Deep River Neutron Monitoring Station hav...
A study of cosmic ray intensity variations has been conducted during 1956–57 at the equatorial mount...