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and a possible cause
Annales Geophysicae, 23, 1917–1930, 2005
SRef-ID: 1432-0576/ag/2005-23-1917
? European Geosciences Union 2005
Annales
Geophysicae
Transpolar aurora: time evolution, associated convection patterns,
and a possible cause
L. G. Blomberg
1
, J. A. Cumnock
1,2
, I. I. Alexeev
3
, E. S. Belenkaya
3
, S. Yu. Bobrovnikov
3
, and V. V. Kalegaev
3
1
Alfve?n Laboratory, Royal Institute of Technology, Stockholm, Sweden
2
Center for Space Sciences, University of Texas at Dallas, USA
3
Skobeltsyn Institute of Nuclear Physics, Moscow State University, Russia
Received: 22 April 2004 – Revised: 11 May 2005 – Accepted: 17 May 2005 – Published: 28 July 2005
Abstract. We present two event studies illustrating the de-
tailed relationships between plasma convection, field-aligned
currents, and polar auroral emissions, as well as illustrat-
ing the influence of the Interplanetary Magnetic Field’s y-
component on theta aurora development. The transpolar arc
of the theta aurorae moves across the entire polar region and
becomes part of the opposite side of the auroral oval. Elec-
tric and magnetic field and precipitating particle data are pro-
vided by DMSP, while the POLAR UVI instrument provides
measurements of auroral emissions. Ionospheric electrostatic
potential patterns are calculated at different times during the
evolution of the theta aurora using the KTH model. These
model patterns are compared to the convection predicted by
mapping the magnetopause electric field to the ionosphere
using the Paraboloid Model of the magnetosphere. The
model predicts that parallel electric fields are set up along
the magnetic field lines projecting to the transpolar aurora.
Their possible role in the acceleration of the auroral electrons
is discussed.
Keywords. Ionosphere (Plasma convection; Polar iono-
sphere) – Magnetospheric physics (Magnetosphere-
ionosphere interactions)
1 Introduction
The global distribution of the aurora has a qualitative as well
as a quantitative dependence on the interplanetar
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