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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Peculiarities of VLF wave propagation in the Earth's magnetosphere in the presence of artificial large-scale inhomogeneity
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Peculiarities of VLF wave propagation in the Earth's magnetosphere in the presence of artificial large-scale inhomogeneity

机译:在人工大规模不均匀性存在下,地球磁层中VLF波传播的特性

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We study specific features of VLF waves propagation in the Earth's ionosphere and magnetosphere in the presence of large-scale field-aligned plasma inhomogeneities (ducts). These inhomogeneities can, e.g., be formed during the ionosphere heating by high-power HF facilities such as High Frequency Active Auroral Research Program and Sura. They can extend up to altitudes of several thousand kilometers along geomagnetic field lines and have transverse scales of about 1 degrees determined by the heated region scale. We analyze ray trajectories of VLF waves with frequencies of 1 to 15kHz starting from about 100km altitude and use the plasma parameters obtained within the framework of the SAMI2 simulation model (Huba et al., 2000). This model employs MHD equations for thermal plasma and allows one to obtain the plasma parameters along the entire magnetic flux tube in a fixed meridional plane. By knowing the ray trajectories, we calculate and compare the amplitude variation along the ray paths for the cases of unperturbed and heated ionosphere. We show that the presence of a large-scale density disturbance produced by the HF heating can lead to significant changes of wave propagation trajectories. In particular, efficient guiding of VLF waves in this region can take place, which in turn can result in the appearance of several wave focusing regions and a drastic local increase of the VLF wave amplitude in these regions (up to approximate to 10 times as compared to the case of unperturbed plasma). The number of focusing regions is determined by an extension of an artificial duct along the geomagnetic field.
机译:我们在大规模场对齐等离子体不均匀性(管道)存在下,研究了地球电离层和磁层中VLF波传播的特定特征。这些不均匀性可以例如通过高功率HF设施的电离层加热形成,例如高频有源极光研究计划和Sura。它们可以沿着地磁场线延伸到几千公里的海拔高度,并且具有由加热区域规模确定的约1度的横向尺度。我们分析VLF波的射频轨迹,频率为1到15kHz,从大约100km高度开始,使用Sami2仿真模型框架内获得的等离子体参数(Huba等,2000)。该模型采用热等离子体的MHD方程,并且允许其中沿着固定的子午线沿整个磁通管获得等离子体参数。通过了解光线轨迹,我们计算并比较沿着射线路径的幅度变化,以便不受干扰和加热电离层的情况。我们表明,通过HF加热产生的大规模密度扰动的存在可能导致波传播轨迹的显着变化。特别地,可以进行该区域中的VLF波的有效引导,这又可以导致几个波聚焦区域的外观和这些区域中的VLF波幅度的急剧局部增加(比较近似为10次)到了不受干扰的等离子体的情况)。聚焦区域的数量由沿着地磁场的人造管道的延伸来确定。

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