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Long-term changes in indices of geomagnetic activity at the auroral station Sodankylä
Authors:D Martini  K Mursula  T Ulich  VS Pandey  K-H Kim  D-H Lee
Institution:1. School of Space Research, Kyung Hee University, Yongin, Gyeonggi-Do 446-701, Republic of Korea;2. Department of Physics, University of Oulu, P.O. Box 3000, 90014 Oulu, Finland;3. Sodankylä Geophysical Observatory, Tähteläntie 62, 99600 Sodankylä, Finland
Abstract:Here we compare the traditional analog measure of geomagnetic activity, Ak, with the more recent digital indices of IHV and Ah based on hourly mean data, and their derivatives at the auroral station Sodankylä. By this selection of indices we study the effects of (i) analog vs. digital technique, and (ii) full local-time vs. local night-time coverage on quantifying local geomagnetic activity. We find that all other indices are stronger than Ak during the low-activity cycles 15–16 suggesting an excess of very low scalings in Ak at this time. The full-day indices consistently depict stronger correlation with the interplanetary magnetic field strength, while the night-time indices have higher correlation with solar wind speed. The Ak index correlates better with the digital indices of full-day coverage than with any night-time index. However, Ak depicts somewhat higher activity levels than the digital full-day indices in the declining phase of the solar cycle, indicating that, due to their different sampling rates, the latter indices are less sensitive to high-frequency variations driven by the Alfvén waves in high-speed streams. On the other hand, the night-time indices have an even stronger response to solar wind speed than Ak. The results strongly indicate that at auroral latitudes, geomagnetic indices with different local time coverage reflect different current systems, which, by an appropriate choice of indices, allows studying the century-scale dynamics of these currents separately.
Keywords:Geomagnetic activity  Geomagnetic indices  Long-term change  Solar wind parameters  Solar activity
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