Abstract
We consider the gradient-current instability of an inhomogeneous magnetoactive plasma in the approximation of double-fluid magnetohydrodynamics. Unlike the known gradient-drift and current-convective instabilities, the gradient-current instability is related to generation of nonpotential quasistatic electric fields polarized orthogonal to the external magnetic field B 0 and excited by eddy currents whose density vector lies in the plane passing through the vectors of the magnetic field B 0 and large-scale electron-density gradient. It is shown that in the high-latitude upper ionosphere, in the regions containing large-scale currents flowing in and out of the ionosphere along the magnetic field, the gradient-current instability can lead to the appearance of sheet-like irregularities extended predominantly in the plane passing through the geomagnetic-field and regular plasma-drift velocity vectors.
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Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Radiofizika, Vol. 48, No. 7, pp. 574–587, August 2005.
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Myasnikov, E.N. On the Gradient-Current Mechanism of Formation of the Irregular Structure of the High-Latitude Upper Ionosphere. Radiophys Quantum Electron 48, 510–521 (2005). https://doi.org/10.1007/s11141-005-0095-5
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DOI: https://doi.org/10.1007/s11141-005-0095-5