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Ion temperature anisotropy effects on the dispersion relation and threshold conditions of a sheared current-driven electrostatic ion-acoustic instability with applications to the collisional high-latitude F-region

Published online by Cambridge University Press:  04 August 2014

Patrick J.G. Perron ,
J.-M. Noël ,
J.-P. St-Maurice  and
K. Kabin
Patrick J.G. Perron*
Affiliation:
Department of Physics, Royal Military College of Canada, Kingston, Ontario, CanadaK7K 7B4
J.-M. Noël
Affiliation:
Department of Physics, Royal Military College of Canada, Kingston, Ontario, CanadaK7K 7B4
J.-P. St-Maurice
Affiliation:
Institute of Space and Atmospheric Studies and Department of Physics and Engineering Physics, University of Saskatchewan, Saskatoon, Saskatchewan, CanadaS7N 5A2
K. Kabin
Affiliation:
Department of Physics, Royal Military College of Canada, Kingston, Ontario, CanadaK7K 7B4
*
†Email address for correspondence: patrick.perron@rmc.ca
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Abstract

Plasma instabilities play a important role in producing small-scale irregularities in the ionosphere. In particular, current-driven electrostatic ion-acoustic (CDEIA) instabilities contribute to high-latitude F-region electrodynamics. Ion temperature anisotropies with enhanced perpendicular temperature often exist in the high-latitude F-region. In addition to temperature anisotropies, ion velocity shears are observed near auroral arc edges, sometimes coexisting with thermal ion upflow processes and field-aligned currents (FAC). We investigated whether ion temperature anisotropy lowers the threshold conditions required for the onset of sheared CDEIA instabilities. We generalised a dispersion relation to include ion thermal anisotropy, finite Larmor radius corrections and collisions. We derived new fluid-like analytical expressions for the threshold conditions required for instability that depend explicitly on ion temperature anisotropy. We studied how the instability threshold conditions vary as a function of the wave vector direction in both fluid and kinetic regimes. We found that, despite the dampening effect of collisions on ion-acoustic waves, ion temperature anisotropy lowers in some cases the threshold drift requirements for a large range of oblique wave vector angles. More importantly, realistic ion temperature anisotropies contribute to reducing the instability threshold velocity shears that are associated with small drift thresholds, for modes propagating almost perpendicularly to the geomagnetic field. Small shear thresholds that seem to be sustainable in the ionospheric F-region are obtained for low-frequency waves. Such instabilities could play a role in the direct generation of field-aligned irregularities in the collisional F-region that could be observed with the Super Dual Auroral Radar Network (SuperDARN) array of high-frequency radars. These modes would be very sensitive to the radar probing direction since they are restricted to very narrow angular intervals. The ion temperature anisotropy is an important parameter that needs to be considered in the studies of sheared and collisional CDEIA waves and instabilities in the high-latitude F-region.

Type
Research Article
Information
Journal of Plasma Physics , Volume 81 , Issue 1 , January 2015 , 905810112
Copyright
Copyright © Cambridge University Press 2014 

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References

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