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Physical Methods for the Separation of the Contributions to the Earth-Space Cross-Polarization Discrimination Using Single-Polarized Satellite Beacon Signals

机译:使用单极化卫星信标信号分离对地球-空间交叉极化的贡献的物理方法

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摘要

The satellite communication systems employing either frequency-reuse schemes and/or polarization diversity to improve spectral efficiency are compromised by depolarization-induced interference due to both rain droplets and aloft ice particles. Any development toward an integrated physical model for depolarization will necessarily require the separation of its different contributions. This task was done in the past using dual-polarized satellite beacon signals that have not been available recently. On the other hand, single-polarized satellite beacon signals are worldwide accessible; therefore, the use of alternative techniques to assess the propagation channel properties is mandatory to unlock the advance of the depolarization studies. Two physical methods able to retrieve ice and rain contributions to total depolarization from single-polarized satellite beacon signals are here described, applied and validated on one full year of measurements carried out at Ka-band.
机译:采用频率复用方案和/或极化分集来提高频谱效率的卫星通信系统,由于雨滴和高空冰粒引起的去极化引起的干扰而受到损害。向去极化的综合物理模型的任何发展都将需要分离其不同的贡献。过去使用最近尚未使用的双极化卫星信标信号来完成此任务。另一方面,单极化卫星信标信号可在全球范围内使用;因此,必须使用替代技术来评估传播通道的性能,以解锁去极化研究的进展。本文描述了两种能够从单极化卫星信标信号中获取冰和雨对总去极化的贡献的物理方法,这些方法在Ka波段进行的整整一年的测量中得到了应用和验证。

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