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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 16, issue 12
Ann. Geophys., 16, 1573–1579, 1998
https://doi.org/10.1007/s00585-998-1573-9
© European Geosciences Union 1998
Ann. Geophys., 16, 1573–1579, 1998
https://doi.org/10.1007/s00585-998-1573-9
© European Geosciences Union 1998

  31 Dec 1998

31 Dec 1998

Longitudinal (UT) effect in the onset of auroral disturbances over two solar cycles as deduced from the AE-index

L. A. Hajkowicz L. A. Hajkowicz
  • Department of Physics, University of Queensland, Qld. 4072, Australia

Abstract. Statistical study on the universal time variations in the mean hourly auroral electrojet index (AE-index) has been undertaken for a 21 y period over two solar cycles (1957–1968 and 1978–1986). The analysis, applied to isolated auroral substorm onsets (inferred from rapid variations in the AE-index) and to the bulk of the AE data, indicates that the maximum in auroral activity is largely confined to 09–18 UT, with a distinct minimum at 03–06 UT. The diurnal effect was clearly present throughout all seasons in the first cycle but was mainly limited to northern winter in the second cycle. Severe storms (AE > 1000 nT) tended to occur between 9–18 UT irrespective of the seasons whereas all larger magnetic disturbances (AE > 500 nT) tended to occur in this time interval mostly in winter. On the whole the diurnal trend was strong in winter, intermediate at equinox and weak in summer. The implication of this study is that Eastern Siberia, Japan and Australia are mostly at night, during the period of maximum auroral activity whereas Europe and Eastern America are then mostly at daytime. The minimum of auroral activity coincides with near-midnight conditions in Eastern America. It appears that the diurnal UT distribution in the AE-index reflects a diurnal change between interplanetary magnetic field orientation and the Earth's magnetic dipole inclination.

Key words. Ionosphere (auroral ionosphere) · Magnetospheric physics (auroral phenomena; storms and substorms).

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