1971•Journal of Geophysical Research AtmospheresRequires access

Topside current instabilities

J. M. Kindel, Charles F. Kennel

Open publisher page 896 citations

Abstract

Both the electrostatic ion acoustic and ion cyclotron waves can be unstable to field-aligned currents comparable to those expected in the auroral zone. However, for a wide range of conditions, the ion cyclotron wave is unstable to the smaller current. In this paper, both instabilities are studied in single and multi-ion plasmas. Profiles of critical current versus height indicate that, as they flow through the topside ionosphere, field-aligned currents of 109–10 electrons/cm2 sec (at 200 km) will destabilize various ion cyclotron waves.

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What this paper is about

Both the electrostatic ion acoustic and ion cyclotron waves can be unstable to field-aligned currents comparable to those expected in the auroral zone. However, for a wide range of conditions, the ion cyclotron wave is unstable to the smaller current. In this paper, both instabilities are studied in single and multi-ion plasmas. Profiles of critical current versus height indicate that, as they flow through the topside ionosphere, field-aligned currents of 109–10 electrons/cm2 sec (at 200 km) will destabilize various ion cyclotron waves.

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Available abstract

Both the electrostatic ion acoustic and ion cyclotron waves can be unstable to field-aligned currents comparable to those expected in the auroral zone. However, for a wide range of conditions, the ion cyclotron wave is unstable to the smaller current. In this paper, both instabilities are studied in single and multi-ion plasmas. Profiles of critical current versus height indicate that, as they flow through the topside ionosphere, field-aligned currents of 109–10 electrons/cm2 sec (at 200 km) will destabilize various ion cyclotron waves.

Key concepts: Cyclotron, Ion, Ionosphere, Physics, Current (fluid), Plasma, Atomic physics, Electron

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