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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 29, issue 4
Ann. Geophys., 29, 673–678, 2011
https://doi.org/10.5194/angeo-29-673-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
Ann. Geophys., 29, 673–678, 2011
https://doi.org/10.5194/angeo-29-673-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

  14 Apr 2011

14 Apr 2011

Magnetic local time dependence of geomagnetic disturbances contributing to the AU and AL indices

S. Tomita1, M. Nosé1, T. Iyemori1, H. Toh1, M. Takeda1, J. Matzka2, G. Bjornsson3, T. Saemundsson3, A. Janzhura4, O. Troshichev4, and G. Schwarz5 S. Tomita et al.
  • 1Graduate School of Science, Kyoto University, Japan
  • 2DTU Space, Technical University of Denmark, Denmark
  • 3University of Iceland, Iceland
  • 4Arctic and Antarctic Research Institute, Russia
  • 5Geological Survey of Sweden, Sweden

Abstract. The Auroral Electrojet (AE) indices, which are composed of four indices (AU, AL, AE, and AO), are calculated from the geomagnetic field data obtained at 12 geomagnetic observatories that are located in geomagnetic latitude (GMLAT) of 61.7°–70°. The indices have been widely used to study magnetic activity in the auroral zone. In the present study, we examine magnetic local time (MLT) dependence of geomagnetic field variations contributing to the AU and AL indices. We use 1-min geomagnetic field data obtained in 2003. It is found that both AU and AL indices have two ranges of MLT (AU: 15:00–22:00 MLT, ~06:00 MLT; and AL: ~02:00 MLT, 09:00–12:00 MLT) contributing to the index during quiet periods and one MLT range (AU: 15:00–20:00 MLT, and AL: 00:00–06:00 MLT) during disturbed periods. These results are interpreted in terms of various ionospheric current systems, such as, Sqp, Sq, and DP2.

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