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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 36, issue 5 | Copyright
Ann. Geophys., 36, 1361-1391, 2018
https://doi.org/10.5194/angeo-36-1361-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Regular paper 17 Oct 2018

Regular paper | 17 Oct 2018

Characteristics of the electrojet during intense magnetic disturbances

Liudmila I. Gromova1, Matthias Förster2,3, Yakov I. Feldstein1, and Patricia Ritter2 Liudmila I. Gromova et al.
  • 1Institute of Terrestrial Magnetism, Ionosphere, and Radiowave Propagation of the Russian Academy of Sciences (IZMIRAN), 142090 Troitsk, Moscow region, Russia
  • 2Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, 14473 Potsdam, Germany
  • 3Max Planck Institute for Solar System Research, 37077 Göttingen, Germany

Abstract. Hall current variations in different time sectors during six magnetic storms from the summer seasons in 2003 and 2005 (Ritter, 2018) are examined, namely three storms in the day–night meridional sector and three storms in the dawn–dusk sector. The sequence of the phenomena, their structure and positions, and the strength of the polar (PE) and the auroral (AE) Hall electrojets were investigated using scalar magnetic field measurements obtained from the CHAllenging Minisatellite Payload (CHAMP) satellite in accordance with the study of Ritter et al. (2004a). We analyzed the correlations of the PE and AE as well as the obtained regression relations of the magnetic latitude MLat and the electrojet current intensity I with auroral and ring current activity, the interplanetary magnetic field, and the Newell et al. (2007) coupling function for the state of the solar wind. The following typical characteristics of the electrojets were revealed:

The PE appears in the daytime sector at MLat ∼ 80°–73°, with a westward or an eastward direction depending on the interplanetary magnetic field (IMF) By component (By < 0nT or By > 0nT). Changes in the current flow direction in the PE can occur repeatedly during the storm, but only due to changes in the IMF By orientation. The PE increases with the intensity of the IMF By component from I ∼ 0.4Am−1 for By ∼ 0nT up to I ∼ 1.0Am−1 for By ∼ 23nT. The MLat position of the PE does not depend on the direction and intensity of the By component.

There is no connection between MLat and I in the PE and the symmetric part of the magnetospheric ring current (index SymH). There is a correlation between I in the PE and the AsyH index, but only a very weak interconnection of this index with the MLat of the PE.

Substorms occurring before the storm's main phase are accompanied by the appearance of an eastward electrojet (EE) at MLat ∼ 64° as well as that of a westward electrojet (WE). In the nighttime sector, a WE appears at MLat ∼ 64°. During the main phase both electrojets persist. The daytime EE and the nighttime WE shift toward sub-auroral latitudes of MLat ∼ 56° and grow in intensity up to I ∼ 1.5Am−1. The WE is then located about 6° closer to the pole than the EE during evening hours and about 2°–3° closer during daytime hours.

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Short summary
Hall current variations in different time sectors during six magnetic storms of the summer seasons in 2003 and 2005 are examined. The sequence of the phenomena, their structure, positions and the strength of the polar and the auroral Hall electrojets were investigated using scalar magnetic field measurements obtained from the CHAMP satellite. We analyzed the correlations and the regression relations of the electrojets with auroral and ring current activity, the IMF, and solar wind parameters.
Hall current variations in different time sectors during six magnetic storms of the summer...
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