Anomalous resistivity in the geomagnetic tail region

Details Anomalous resistivity in the geomagnetic tail region Anomalous resistivity in the geomagnetic tail region

Nov 1978

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1978p%26ss...26.1033p&link_type=abstract

Planetary and Space Science, Volume 26, Issue 11, p. 1033-1035.

Physics

Scientific paper

The beam cyclotron instability and electron acoustic instability, driven by cross-tail current and inhomogeneity in density and magnetic field, are found to be unstable in the earth's magnetic tail region. The anomalous resistivities due to these instabilities are found to be of the order of (10-1-10-3)Ωe-1 (Ωe being the electron gyro frequency). It is also suggested that the non-linear saturation of the beam cyclotron instability may lead to conditions favourable for exciting ion acoustic instability.

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