We report a characteristic bifurcation of the cusp aurora in associati
on with northward transitions of the interplanetary magnetic field (IM
F), leading to the coexistence of latitudinally separated forms, calle
d types I and 2. In the northernmost form (type 2), which is located a
t similar to 77 - 79 degrees MLAT, there appears a sequence of auroral
brightenings at the poleward boundary of the preexisting luminosity.
Each brightening is followed by equatorward motion and fading of the i
ndividual forms. Furthermore, coherent intensity variations of the two
latitudinally separated forms are often observed. This is documented
by three case examples. The most active phase of the type 2 aurora is
observed during intervals of 15 - 20 min duration following northward
turnings of the IMF and with nonzero IMF B-y component, corresponding
to the transition state before a new equilibrium state of solar wind-m
agnetosphere coupling is established. The auroral observations are dis
cussed in relation to theoretical models of ionospheric convection, fi
eld-aligned currents and solar wind-magnetosphere coupling in the pola
r cusp region. The type 2 auroral activity in the north is interpreted
as an ionospheric signature which is directly related to reconnection
between the IMF and the terrestrial lobe field at the high-latitude m
agnetopause, whereas the type 1 aurora is coupled to the low latitude
magnetopause. The coherent activations of the two auroral forms indica
te that the corresponding current systems are strongly coupled at the
ionospheric level.