Excitation of transient lobe cell convection and auroral arc at the cusp poleward boundary during a transition of the interplanetary magnetic field from south to north
Pe. Sandholt et al., Excitation of transient lobe cell convection and auroral arc at the cusp poleward boundary during a transition of the interplanetary magnetic field from south to north, ANN GEOPHYS, 19(5), 2001, pp. 487-493
We document the activation of transient polar arcs emanating from the cusp
within a 15 min long intermediate phase during the transition from a standa
rd two-cell convection pattern, representative of a strongly southward inte
rplanetary magnetic field (IMF), to a "reverse" two-cell pattern, represent
ative of strongly northward IMF conditions. During the 2-3 min lifetime of
the are, its base in the cusp, appearing as a bright spot, moved eastward t
oward noon by similar to 300 km. As the are moved, it left in its "wake" en
hanced cusp precipitation. The polar are is a tracer of the activation of a
lobe convection cell with clockwise vorticity, intruding into the previous
ly established large-scale distorted two-cell pattern, due to an episode of
localized lobe reconnection. The lobe cell gives rise to strong flow shear
(converging electric field) and an associated sheet of outflowing field-al
igned current, which is manifested by the polar are. The enhanced cusp pre
cipitation represents, in our view, the ionospheric footprint of the lobe r
econnection process.