基于热带雨传感器测量数据的毫米波衰减

Lu Li, A. Sali, Sangin Qahtan Wali
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引用次数: 0

摘要

对于热带地区,降雨是毫米波传输衰减的主要因素。本文以马来西亚KLIA雪邦地区为例,通过雨水传感器测量和采集降雨率数据,建立热带地区毫米波降雨衰减的数学模型,通过MATLAB软件模拟计算20-300 GHz不同频率范围内的降雨衰减,重点分析了广泛使用的30-50GHz频段毫米波通信衰减特性。结果表明,降雨速率越大,降雨频率越高,降雨衰减越大。与圆偏振和水平偏振相比,垂直偏振的衰减最小。衰减和衰减速率随频率和降雨速率的增加而增加。其中,在30-50GHz频段,在降雨速率为20-60mm/h时,衰减值在15dB ~ 90dB范围内呈线性变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Attenuation of mmWave Based on Measured Data via Rain Sensor in Tropical Region
For tropical areas, rainfall is the main factor in the attenuation of millimeter wave transmission. This paper considers KLIA Sepang region of Malaysia as an example to measure and collect rainfall rate data via rain sensor, establish a mathematical model for millimeter wave rainfall attenuation in tropical areas, simulate and calculate rainfall attenuation at different frequency ranges of 20-300 GHz through MATLAB software, with emphasis on the analysis of millimeter wave communication attenuation characteristics in the widely used 30-50GHz frequency band. The results show that the greater the rainfall rate, the higher the frequency, and the greater the rainfall attenuation. Moreover, the vertical polarization achieves the lowest attenuation compared circular polarization and horizontal polarization. The attenuation and attenuation rate increase with the increase of frequency and rainfall rate. Specifically, the attenuation value appears linearly in the range of 15dB to 90dB in the rainfall rate of 20-60mm/h for the frequency bands of 30-50GHz.
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