Structure and nature of spectra of the geomagnetic field in the case of very large magnetic storms (13-14 March 1989 and 8-9 Nov. 1991)

Physics

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Energy Spectra, Geomagnetism, Kelvin-Helmholtz Instability, Magnetic Storms, Magnetospheric Instability, Atmospheric Boundary Layer, Magnetic Variations

Scientific paper

Digital magnetic-variation data from polar, auroral, and midlatitude stations indicate that the energy spectra of very large storms have a uniform structure at all latitudes from 20 to 80 deg, with four maxima in the 20-30, 30-40, 40-50, and 50-60 min intervals. It is suggested that the high-frequency maxima arise because of the finite thickness of the low-latitude boundary layer of the magnetosphere on the spectrum of Kelvin-Helmholtz instability waves.

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