Low energy (less than 130 eV) oxygen ions at the geosynchronous orbit during the CDAW 6 event of March 22, 1979

Details Low energy (less than 130 eV) oxygen ions at the geosynchronous orbit during the CDAW 6 event of March 22, 1979 Low energy (less than 130 eV) oxygen ions at the geosynchronous orbit during the CDAW 6 event of March 22, 1979

Feb 1985

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1985jgr....90.1253s&link_type=abstract

Journal of Geophysical Research (ISSN 0148-0227), vol. 90, Feb. 1, 1985, p. 1253-1261. Sponsorship: Swiss National Science Found

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Equatorial Atmosphere, Magnetic Storms, Oxygen Ions, Positive Ions, Satellite Sounding, Space Plasmas, Anisotropic Media, Cold Plasmas, Geos 2 Satellite, Geosynchronous Orbits, Magnetohydrodynamic Flow

Scientific paper

Anisotropic O(+) ions were frequently observed by the GEOS 2 ion composition experiment in the energy range 4-130 eV, during the CDAW 6 event of March 22, 1979. These observations allow the study of the plasma flow in the electric and magnetic fields as known from data of other experiments in the geosynchronous orbit, in the noon, dusk, and midnight sectors. By comparison of these measurements with plasma observations made by the ISEE 2 plasma experiment, at the same local time and at different latitudes, the observation of cold plasma streaming along magnetic field lines from the polar ionosphere to the equatorial magnetosphere is extended from the magnetotail to the near earth equatorial region.

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