Fractals and magnetic storm
Fractal theory is applied in a quantitative analysis of geomagnetic storms. Fractal dimensions (<i>D</i>) of the attractor for storm data from the Beijing observatory (40.0°N, 116.2°E) using several time intervals are calculated. A maximum value of 1.4 has been obtained for a geomagn...
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| Format: | Article |
| Language: | English |
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Copernicus Publications
1996-09-01
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| Series: | Annales Geophysicae |
| Online Access: | https://www.ann-geophys.net/14/888/1996/angeo-14-888-1996.pdf |