Heating of oxygen ions by resonant absorption of Alfven waves in a multicomponent plasma

Physics

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Energy Absorption, Ionospheric Heating, Magnetohydrodynamic Waves, Oxygen Ions, Plasma Resonance, Wave-Particle Interactions, Conics, Coupled Modes, Ion Cyclotron Radiation, Polar Cusps

Scientific paper

The present analysis demonstrates the likelihood that oxygen ions are heated transversely by the large-amplitude Alfvenic fluctuations related to downgoing waves. Alfven waves propagating earthward through a multicomponent plasma are shown to be mode-converted by the inhomogeneous geomagnetic field into O(+) cyclotron waves leading to transverse resonant heating of the O(+) ions. The absorption coefficient at the O(+) gyrofrequency range is studied in the context of the cold-plasma approximation, and two types of downgoing waves are found to play a role in the absorption process. Critical parameters for this process are identified, and comparisons are made to the Viking and DE-1 experimental data. The optimized conditions for oxygen-ion heating are found to be satisfied in the region where the Alfvenic turbulence is accompanied by conics.

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