Abstract
The delicate structure of magnetospheric perturbations in electron fluxes and low-frequency emissions in studied at altitudes of the Intercosmos 19 satellite (500 to 1.000 km) in different sectors of local time on March 22, 1979 (CDAW-6 interval). The specific features of the differential energy spectrs of the electrons of the Earth's outer radiation belt are studied depending on geophysical activity. It is concluded that at the initial phase of substorms a rapid radial diffusion of the electrons inside the magnetosphere up to L ∼ 2 can take place along with the decrease of the electron capture region. Data on particles and waves are used for determining diffusion coefficients.
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