DYNAMICAL AURORAL MORPHOLOGY IN RELATION TO IONOSPHERIC PLASMA CONVECTION AND GEOMAGNETIC-ACTIVITY - SIGNATURES OF MAGNETOPAUSE X-LINE DYNAMICS AND FLUX-TRANSFER EVENTS

Citation
M. Oieroset et al., DYNAMICAL AURORAL MORPHOLOGY IN RELATION TO IONOSPHERIC PLASMA CONVECTION AND GEOMAGNETIC-ACTIVITY - SIGNATURES OF MAGNETOPAUSE X-LINE DYNAMICS AND FLUX-TRANSFER EVENTS, J GEO R-S P, 101(A6), 1996, pp. 13275-13292
Citations number
54
Categorie Soggetti
Geosciences, Interdisciplinary","Astronomy & Astrophysics","Metereology & Atmospheric Sciences
Journal title
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
ISSN journal
21699380 → ACNP
Volume
101
Issue
A6
Year of publication
1996
Pages
13275 - 13292
Database
ISI
SICI code
2169-9380(1996)101:A6<13275:DAMIRT>2.0.ZU;2-J
Abstract
Ground-based observations of auroral, geomagnetic, and radar signature s of solar wind-magnetosphere coupling modes are presented. Two differ ent categories of ionospheric signatures are studied: (1) enhanced geo magnetic deflections and associated equatorward displacements of the c usp/cleft aurora and (2) a sequence of poleward moving amoral and geom agnetic events. It is suggested that signature 1 is mainly caused by d irectional. discontinuities in the interplanetary magnetic held changi ng the solar wind-magnetosphere coupling geometry and that signature 2 is caused by a recurring modulation of the reconnection rate at the d ayside magnetopause (flux transfer events (FTEs)), during the period o f strong coupling. The observed auroral and geomagnetic signatures are placed in the context Of plasma convection, as derived from magnetome ters in Svalbard, Greenland, and Canada, and the European incoherent s catter (EISCAT) radar. A suggestion for an ionospheric current system explaining the sequence of poleward propagating events, i.e., the FTE signatures, is presented.