VLF-ULF范围内各向异性地球-电离层波导的正态波

V. Kirillov, A. E. Pronin
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引用次数: 3

摘要

解决了地球-电离层波导中距离10−1−10 km、频率为10−1−10 Hz的近地水平电偶极子电磁场的测定问题。假定电离层是水平分层和各向异性的,假定地球在某一深度是均匀的,在以下是无限导电的。给出了电磁场在波导模式下的扩展表示。零模被认为是各向异性的。在各向异性电离层的各向同性近似中,由于包含了有效的指数电导率曲线,给出了局域模式。对该模型的垂直偏振和水平偏振的场反射进行了解析描述。在离源很近的地方,解与没有电离层的情况下的已知解一致。已经发现了电离层对近地磁场的影响所起的距离范围。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Normal waves of the anisotropic Earth-ionosphere waveguide in the VLF-ULF range
[1] The problem on determination of the electromagnetic field of a near-Earth horizontal electric dipole in the frequency range 10−1 − 10 Hz at distances 10−1 − 10 km in the Earth–ionosphere waveguide has been solved. The ionosphere is assumed to be horizontally stratified and anisotropic, and the Earth is assumed to be homogeneous to some depth and infinitely conducting below. The representation of the electromagnetic field as expansion in waveguide modes is given. The zero mode is regarded as anisotropic. Local modes are given in the isotropic approximation of the anisotropic ionosphere due to inclusion of an effective exponential conductivity profile. An analytical description of the field reflection for vertical and horizontal polarizations has been obtained for this model. At short distances from the source, the solution coincides with the known solution for the case of the absence of the ionosphere. The range of distances beginning from which the influence of the ionosphere on the near-Earth magnetic field manifests itself has been found.
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