Effect of electron heating on the longitudinal velocities of O(+) ions in magnetic flux tubes

Details Effect of electron heating on the longitudinal velocities of O(+) ions in magnetic flux tubes Effect of electron heating on the longitudinal velocities of O(+) ions in magnetic flux tubes

Sep 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986kosis..24..787g&link_type=abstract

Kosmicheskie Issledovaniia (ISSN 0023-4206), vol. 24, Sept.-Oct. 1986, p. 787-791. In Russian.

Physics

Electron Energy, Ion Motion, Ionospheric Heating, Ionospheric Ion Density, Magnetic Flux, Particle Interactions, Time Dependence, Vertical Distribution

Scientific paper

A self-consistent model was used to account for the effect of electron heating (EH) on longitudinal velocities of O(+) ions in high-latitude geomagnetic flux tubes. An analysis of the height-time dependences of ion velocity and concentration shows that EH can lead to the transport of large fluxes of O(+) ions from the ionosphere to the magnetosphere. At a height of 10,000 km, the O(+) flux in the polar wind reaches a value of 2.2 x 10 to the 6th/sq cm s.

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