Interchange instability in the inner magnetosphere associated with geosynchronous particle flux decreases

Geophysical Research Letters

Volumn 29, Issue 10, 2002, Pages 88-1-88-4

  Sazykin, S ^a   Wolf, R A ^a   Spiro, R W ^a   Gombosi, T I ^b   De Zeeuw, D L ^b   Thomsen, M F ^c  

^a RICE UNIVERSITY   (United States)

^b UNIVERSITY OF MICHIGAN   (United States)

^c LOS ALAMOS NATIONAL LABORATORY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

IONOSPHERE; MAGNETOSPHERE; PLASMA DENSITY; STORMS;

PARTICLE FLUXES;

GEOPHYSICS;

MAGNETOSPHERE;

EID: 0037095898     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2001gl014416     Document Type: Article

References (18)

1. The terrestrial ring current: Origin, formation and decay
2. Comprehensive computational model of Earth's ring current
3. Motions in the magnetosphere of the Earth
4. Quantitative simulation of a magnetospheric substorm 1, Model logic and overview
5. Intense sheared flow as the origin of large-scale undulations of the edge of the diffuse aurora
6. Dominant role of the asymmetric ring current in producing the stormtime Dst
7. Large-amplitude undulations on the equatorward boundary of the diffuse aurora
8. Substorm injection boundaries
9. Isolated cold plasma regions: Observations and their relation to possible production mechanisms
10. On calculating ionospheric conductances from the flux and energy of precipitating electrons
11. Dependence of the large-scale, inner magnetospheric electric field on geomagnetic activity
12. On the magnetospheric interchange instability
13. An observational test of the Tsyganenko (T89a) model of the magnetospheric field
14. Computer simulation of inner magnetospheric dynamics for the magnetic storm of July 29, 1977
15. Extension of convection modeling into the high-latitude ionosphere: Some theoretical difficulties
16. Convective generation of "giant" undulations on the evening diffuse auroral boundary