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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Two-Dimensional Full-Wave Simulation of Whistler Mode Wave Propagation Near the Local Lower Hybrid Resonance Frequency in a Dipole Field
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Two-Dimensional Full-Wave Simulation of Whistler Mode Wave Propagation Near the Local Lower Hybrid Resonance Frequency in a Dipole Field

机译:二维全波仿真惠斯勒波传播模式在当地较低的混合在偶极子共振频率

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摘要

We investigate the propagation of whistler mode waves near the local lower hybrid resonance (LHR) frequency in a dipole field with a two-dimensional full-wave model. First, we run a simulation in which a parallel whistler with frequency above the local LHR frequency is launched at the equatorial region in electron plasma. We find that whistler emission propagates along the dipole field line to a high latitude, turns quasi-electrostatic where the wave frequency is close to the local LHR frequency, and continues to propagate until being absorbed. Then, the proton response is considered. We find that (1) a quasi-electrostatic whistler reflects where the wave frequency is below the local LHR frequency and propagates to a larger L-shell and lower latitude, (2) a strong standing-wave pattern is formed in the LHR reflection region, and (3) the whistler emission turns from right-hand circularly polarized to linearly polarized near the reflection region. Finally, we run a simulation in which a quasi-electrostatic whistler is launched at a high latitude with a small-scale density irregularity added as a depletion to the background plasma. We find that a small portion of quasi-electrostatic whistler energy can be coupled to a parallel whistler, which can propagate to a much lower altitude while most of the wave energy experiences LHR reflection. Moreover, the mode coupling depends on the transverse and longitudinal sizes of the density irregularity. This makes a possible explanation of ground observations of nonducted whistler emission, which could have been reflected in the high-latitude ionosphere and magnetosphere.
机译:我们调查惠斯勒的传播模式波附近的当地较低的混合共振(LHR)一个偶极子场的频率二维全波模型。仿真的并行惠斯勒频率高于当地LHR频率在赤道地区启动电子等离子体。在偶极子场线高纬度,把quasi-electrostatic波频率接近当地的LHR频率,直到被吸收并继续传播。然后,质子反应被认为是。(1) quasi-electrostatic惠斯勒反映波频率低于当地LHR在哪里频率和较大的l层和传播纬度较低,(2)一个强大的驻波模式形成的LHR反射的区域,和(3)惠斯勒从物右旋圆偏振线性偏振反射附近地区。运行一个仿真一个quasi-electrostatic惠斯勒在高纬度和启动小规模的密度不均匀性作为补充道枯竭的背景等离子体。一小部分quasi-electrostatic惠斯勒能量可以被耦合到一个平行的惠斯勒,可以传播到更低的高度吗虽然大多数的波能经历反射。的横向和纵向尺寸密度不均匀性。解释nonducted地面观测的惠斯勒发射,这可能是反映在高纬度地区电离层磁气圈。

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