Fine structure of the preliminary impulse of a sudden storm commencement

Details Fine structure of the preliminary impulse of a sudden storm commencement Fine structure of the preliminary impulse of a sudden storm commencement

Jun 1985

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1985ge%26ae..25..420p&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 25, May-June 1985, p. 420-424. In Russian.

Physics

Fine Structure, Geomagnetic Pulsations, Magnetic Storms, Sudden Storm Commencements, Ground Truth, Magnetospheric Instability, Satellite Observation, Shock Wave Propagation

Scientific paper

The fine structure of preliminary reverse impulses is analyzed on the basis of 200 SSC events recorded during 1965-1979 at the Irkutsk station and special experiments at the meridional chain of stations; a joint analysis of ground and satellite observations of the SSC of July 29, 1977 is also performed. It is shown that the PRI fine structure has the form of a strain of damped oscillations in the Pc2-3 range with a duration not greater than approximately 2 min. The excitation of these oscillations is connected with the propagation of a fast magnetoacoustic wave, generated in the interaction between the interplanetary shock wave and the magnetosphere.

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