A fractal temporal analysis of moderate and intense magnetic storms
In this paper we have studied, in terms of a fractal analysis, the time distribution of Dst peaks associated with Storm Sudden Commencements (SSCs), during the years 1957 and 1978. To ensure a complete set of data, we considered only moderate and strong storms (Dst peaks < - 50 nT) and performed...
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Elsevier Ltd
1997
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| LEADER | 06203caa a22006497a 4500 | ||
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| 003 | AR-BaUEN | ||
| 005 | 20250807114935.0 | ||
| 008 | 190411s1997 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-0043132128 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Osella, Ana María | |
| 245 | 1 | 2 | |a A fractal temporal analysis of moderate and intense magnetic storms |
| 260 | |b Elsevier Ltd |c 1997 | ||
| 270 | 1 | 0 | |m Osella, A.; Departamento de Física, Fac. de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Pab. 1, 1428, Buenos Aires, Argentina |
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| 504 | |a (1976) IAGA Bulletin, (32 F), pp. 53-54 | ||
| 504 | |a (1977) IAGA Bulletin, (32 G), pp. 60-61 | ||
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| 504 | |a (1978) IAGA Bulletin, (32 H), pp. 60-61 | ||
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| 504 | |a Mandelbrot, B., (1982) The Fractal Geometry of Nature, , W. H. Freeman and Co., San Francisco, California | ||
| 504 | |a Robertson, M., Sammis, Ch., Sahimi, M., Martin, A., Fractal analysis of three-dimensional distributions of earthquakes with a percolation interpretation (1995) J. Geophys. Res., 100, pp. 609-620 | ||
| 504 | |a Smalley, R.F., Chatelain, L., Turcotte, D.L., Prévot, R., A fractal approach to the clustering of earthquakes: Applications to the seismicity of the New Hebrides (1987) Bull. Seismol. Soc. Am., 77, pp. 1368-1381 | ||
| 504 | |a Sugiura, M., (1964) Hourly Values of Equatorial Dst for the IGY, Annual International Geophysical Year, 35, p. 9. , Pergamon, New York | ||
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| 504 | |a Turcotte, D., Fractals in geology and geophysics (1989) PAGEOPH, 131, pp. 171-196 | ||
| 506 | |2 openaire |e Política editorial | ||
| 520 | 3 | |a In this paper we have studied, in terms of a fractal analysis, the time distribution of Dst peaks associated with Storm Sudden Commencements (SSCs), during the years 1957 and 1978. To ensure a complete set of data, we considered only moderate and strong storms (Dst peaks < - 50 nT) and performed three analyses, one including all these events and then each one, moderate and strong, separately. Using a 1D box counting technique, the fractal dimension was determined within the ranges of time scales over which good fits were obtained. Similar results have been observed for the different sets of data. In all the cases a strong clustering has been determined for ranges of scale series between 1 month and 1 yr, showing a non-random contribution in the generation of storms with sudden commencements, which are usually associated to a stochastic behavior. Copyright © 1996 Elsevier Science Ltd. |l eng | |
| 593 | |a Departamento de Física, Fac. de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Pab. 1, 1428, Buenos Aires, Argentina | ||
| 593 | |a Departamento de Geología, Fac. de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Pab. 2, 1428, Buenos Aires, Argentina | ||
| 700 | 1 | |a Favetto, Alicia Beatriz | |
| 700 | 1 | |a Silbergleit, V. | |
| 773 | 0 | |d Elsevier Ltd, 1997 |g v. 59 |h pp. 445-451 |k n. 4 |p J. Atmos. Sol.-Terr. Phys. |x 13646826 |w (AR-BaUEN)CENRE-5432 |t Journal of Atmospheric and Solar-Terrestrial Physics | |
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