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