Ion ring current during magnetic disturbances according to observations in geostationary orbit. I - The dynamics during moderate storms

Details Ion ring current during magnetic disturbances according to observations in geostationary orbit. I - The dynamics during moderate storms Ion ring current during magnetic disturbances according to observations in geostationary orbit. I - The dynamics during moderate storms

Jul 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987kosis..25..599v&link_type=abstract

Kosmicheskie Issledovaniia (ISSN 0023-4206), vol. 25, July-Aug. 1987, p. 599-605. In Russian.

Computer Science

Earth Ionosphere, Magnetic Storms, Ring Currents, Flux Density, Hydrogen Ions, Synchronous Satellites

Scientific paper

An analysis is made of data on fluxes of H(+) ions and ions of the (C, N, O) group with different charges, obtained on the Gorizont (1985-07A) geostationary satellite during three moderate magnetic disturbances with Dst-variation amplitudes of several tens of nTl. It is shown that geomagnetic storms with pronounced main phases are accompanied by the intense injection of H(+) and (N, O)(2+) ion fluxes in the absence of appreciable increases in the fluxes of multiply charged (C, N, O) ion fluxes with energies of the order of 10 keV/e. These results indicate that the ionospheric plasma is the main source of ring-current particles in this energy range.

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