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Nonlin. Processes Geophys., 16, 691-698, 2009
www.nonlin-processes-geophys.net/16/691/2009/
doi:10.5194/npg-16-691-2009
© Author(s) 2009. This work is distributed
under the Creative Commons Attribution 3.0 License.


Variability of magnetic field spectra in the Earth's magnetotail

A. A. Petrukovich and D. V. Malakhov
Space Research Institute, 84/32 Profsoyuznaya st., Moscow, 117997, Russia
Moscow Institute of Physics and Technology, Moscow, Russia

Abstract. We investigate the variability of magnetic fluctuation spectra below 1 Hz in the Earth's plasma sheet using specially selected long observation intervals by Geotail spacecraft. The spectra can be generally described by a negative power law with two kinks. The range between kinks ~0.02–0.2 Hz has the most stable power law index ~2.4–2.6. Indices at the lower and the higher frequencies are more variable and generally increase with power of fluctuations. In the sub-second range fluctuations are strongly localized and indices are closer to 3. At the lower-frequency end indices are about 1.5. The lower kink is usually well defined on average spectra and its frequency tends to increase with activity. Combination of spectrum index α and fractal dimension δ is expected to follow the Berry relation α+2δ=5, but actually is ~5.5.

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Citation: Petrukovich, A. A. and Malakhov, D. V.: Variability of magnetic field spectra in the Earth's magnetotail, Nonlin. Processes Geophys., 16, 691-698, doi:10.5194/npg-16-691-2009, 2009.   Bibtex   EndNote   Reference Manager    XML
 

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