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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 32, issue 6
Ann. Geophys., 32, 609-622, 2014
https://doi.org/10.5194/angeo-32-609-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
Ann. Geophys., 32, 609-622, 2014
https://doi.org/10.5194/angeo-32-609-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Regular paper 04 Jun 2014

Regular paper | 04 Jun 2014

Determining the boundaries of the auroral oval from CHAMP field-aligned current signatures – Part 1

C. Xiong2,1, H. Lühr1, H. Wang2, and M. G. Johnsen3 C. Xiong et al.
  • 1Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
  • 2Department of Space Physics, College of Electronic Information, Wuhan University, 430079 Wuhan, China
  • 3Tromsø Geophysical Observatory, Faculty of Science and Technology, University of Tromsø, Tromsø, Norway

Abstract. In this paper we present the first statistical study on auroral oval boundaries derived from small- and medium-scale field-aligned currents (FACs, < 150 km). The dynamics of both the equatorward and poleward boundaries is deduced from 10 years of CHAMP (CHAllenging Minisatellite Payload) magnetic field data (August 2000–August 2010). The approach for detecting the boundaries from FACs works well under dark conditions. For a given activity level the boundaries form well-defined ellipses around the magnetic pole. The latitudes of the equatorward and poleward boundaries both depend, but in different ways, on magnetic activity. With increasing magnetic activity the equatorward boundary expands everywhere, while the poleward boundary shows on average no dependence on activity around midnight, which seems to be stationary at a value of about 72° Mlat. Functional relations between the latitudes of the boundaries and different magnetic activity indices have been tested. Best results for a linear dependence are derived for both boundaries with the dayside merging electric field. The other indices, like the auroral electrojet (AE) and disturbance storm time (Dst) index, also provide good linear relations but with some caveats. Toward high activity a saturation of equatorwards expansion seems to set in. The locations of the auroral boundaries are practically independent of the level of the solar EUV flux and show no dependence on season.

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