INCREASED MAGNETIC STORM ACTIVITY FROM 1868 TO 1995

Citation
Ma. Clilverd et al., INCREASED MAGNETIC STORM ACTIVITY FROM 1868 TO 1995, Journal of atmospheric and solar-terrestrial physics, 60(10), 1998, pp. 1047-1056
Citations number
18
Categorie Soggetti
Metereology & Atmospheric Sciences","Geochemitry & Geophysics
Volume
60
Issue
10
Year of publication
1998
Pages
1047 - 1056
Database
ISI
SICI code
Abstract
The aa index provides the longest continuous data set which can be use d in the analysis of magnetospheric and ionospheric phenomenology. All phases of the solar cycle show increases in activity since cycle 14. The activity increase does not appear to be associated with any instru mental, ionospheric or magnetospheric effects. Barely significant effe cts (in terms of the results presented in this paper) have been identi fied in the long-term change in magnetic latitude of the observatory s ites, the positions of high-latitude ionospheric features such as the cusp, and ionospheric Pedersen and Hall conductivities due to changing magnetic field orientation and strength. The prime cause of the chang e in geomagnetic activity is an increase in solar activity. The number of storms at solar minimum has typically increased by 40% more than t he other phases. This is principally due to increased recurrent storm activity to such an extent that conditions at minimum in recent cycles could be thought of as being more representative of the declining pha se. (C) 1998 Elsevier Science Ltd. All rights reserved.