Fractals and magnetic storm

Details Fractals and magnetic storm Fractals and magnetic storm

Sep 1996

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1996angeo..14..888w&link_type=abstract

Annales Geophysicae, vol. 14, Issue 9, pp.888-892

Physics

2

Scientific paper

Fractal theory is applied in a quantitative analysis of geomagnetic storms. Fractal dimensions (D) 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 geomagnetic storm; on quite days the dimension is only slightly larger than 0.5. Data from two storms are analyzed here. Results show that a combination of both D and the magnetic index, k, can perhaps describe the degree of solar disturbance better than the single parameter k.

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