Pe. Sandholt et al., Dayside auroral bifurcation sequence during B-y-dominated interplanetary magnetic field: Relationship with merging and lobe convection cells, J GEO R-S P, 106(A8), 2001, pp. 15429-15444
We report observations in the cusp region of synchronous activations of lat
itudinally separated auroral forms ("bifurcations") occurring in a sequence
and interpret the observations in terms of an intermittent magnetic reconn
ection process at the dayside magnetopause proceeding in a wave-like manner
from lower to higher latitudes, The observations refer to a B-y-dominated
interplanetary magnetic field (IMF) orientation, Optical auroral observatio
ns are combined with radar observations of ionospheric ion drift to illustr
ate the association between the aurora and plasma convection in two cases r
epresenting positive and negative IMF B-y conditions. In the meridian photo
meter scans, each individual event in the sequence appeared as an initial b
rightening in the south (type 1), followed by a second brightening/expansio
n farther to the north (type 2). The events occurring during all eastward p
ointing (B-y>0) IMF are observed typically to expand westward across the 12
00 magnetic local time meridian, from the postnoon to the prenoon side. The
higher-latitude, type 2 activity is associated with strong westward convec
tion, which we identify to be part of a lobe cell, while the equatorward bo
undary intensifications (type 1) occur in the region of a merging cell, dis
torted by the prevailing IMF B-y condition. The auroral sequence consists o
f several paired activation events, typically recurring at similar to 5- to
10-min intervals, and each individual event lasting similar to 10 min. The
ion drift observations are found to be consistent with recent MHD modeling
results on IMF magnetosphere interconnection geometry and the associated c
omposite pattern of merging and lobe convection cells in the cusp region, T
he ground observations reveal the intermittent nature of two components of
cusp region particle precipitation and the association between the correspo
nding type 1 and 2 auroras and merging and lobe convection cells, respectiv
ely.