Attenuation of Terahertz Waves by Wet Sn Ow, Dry Snow and Rain

Yasith Amarasinghe, Wei Zhang, Rui Zhang, D. Mittleman, Jianjun Ma
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Abstract

The technology of terahertz (THz) waves offer wide bandwidth and high capacity for future wireless communications. However, THz waves also suffer from high sensitivity to adverse weather conditions when propagating in the near-surface atmosphere. There have been several systematic studies conducted on this under different weather conditions such as rain, fog, haze, cloud and air turbulence. In particular, several investigations of the scattering performance of terahertz waves in snow have been reported [1]. But, there is still a lack of systematic studies because of the difficulties in measurements and characterizations due to the complicate shapes of snow particles. Therefore, a combined approach relying on both theoretical models and case studies is valuable. In this work, we combine meteorological data and Mie scattering theory to investigate the scattering behavior of THz waves in falling snow and in a snow layer. The theoretical results are in rough qualitative agreement with the experimental data when gaseous attenuation and scintillation effect are not considered. Compared with the attenuation by rain, the THz signal suffers higher loss when propagates in dry and wet snow for frequencies above 200 GHz. Signal loss in dry snow layer is mainly attributed to scattering effects because of the low water content, and it doesn't change when the temperature is reduced from 0 to -20 oC. The absorption effect becomes more serious when snow wetness increases, but the scattering effect is largely unaffected by water content.
湿雪、干雪和雨对太赫兹波的衰减
太赫兹(THz)波技术为未来的无线通信提供了宽带宽和高容量。然而,太赫兹波在近地表大气中传播时,对恶劣天气条件也有很高的敏感性。在不同的天气条件下,如雨、雾、霾、云和空气湍流,已经进行了一些系统的研究。特别是,一些关于太赫兹波在雪中的散射性能的研究已经被报道[1]。但是,由于雪粒子形状复杂,测量和表征困难,目前还缺乏系统的研究。因此,依靠理论模型和案例研究相结合的方法是有价值的。本文结合气象资料和Mie散射理论,研究了降雪和雪层中太赫兹波的散射特性。在不考虑气体衰减和闪烁效应的情况下,理论结果与实验数据在定性上基本一致。与雨的衰减相比,太赫兹信号在干燥和潮湿的雪中传播时,频率在200 GHz以上时损失更大。干雪层的信号损失主要是由于含水量低造成的散射效应,当温度从0℃降至-20℃时,信号损失基本不变。随着雪湿度的增加,吸收效应变得更加严重,而散射效应基本上不受含水量的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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