Ion Bernstein instability in the terrestrial magnetosphere: Linear dispersion theory
Ion Bernstein instability in the terrestrial magnetosphere: Linear dispersion theory
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DOI:
10.1029/2010ja015965
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发表时间:
2010-12
影响因子:
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通讯作者:
S. Gary;Kaijun Liu;D. Winske;R. Denton
中科院分区:
文献类型:
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作者:
S. Gary;Kaijun Liu;D. Winske;R. Denton
[1] Linear kinetic dispersion theory for electromagnetic fluctuations in a homogeneous, magnetized, collisionless plasma is used to study the properties of an ion Bernstein mode instability driven by a proton velocity distribution fp(v) such that ∂fp(ν⊥)/∂ν⊥ > 0, where ⊥ denotes directions perpendicular to the background magnetic field Bo. Here fp(v) = f1(ν) − f2(ν), where f1 and f2 are Maxwellian velocity distributions with slightly different densities and temperatures; plasma parameters are taken from magnetospheric observations. Then the growth rate of this instability has relative maxima at ωr ≃ nΩp, where n = 1, 2, 3, … and Ωp is the proton cyclotron frequency; wave vector k at 0 < k∥ ≪ k⊥, where ∥ and ⊥ denote the directions parallel and perpendicular to Bo; and wavelengths of the order of or smaller than the proton gyroradius. The maximum instability growth rate is a monotonically decreasing function of the electron-to-proton temperature ratio but has its largest value at an intermediate value of the proton β (∼0.5 for the parameters considered here).