CLOUD ATTENUATION AT Ka, Q AND W BANDS BASED ON RADIOSOUNDINGS DURING RAINY AND NON-RAINY SEASONS IN CENTRAL ANDES: A STUDY IN EL ALTO, BOLIVIA

Alejandro Garcia, G. Siles, Juan Pablo Arciénega, Yasmín Balderrama
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Abstract

Cloud attenuation in satellite communication systems becomes a relevant issue as the frequency increases, and thus, it has to be taken into account when link availability is being calculated. This atmospheric impairment is a variable atmospheric phenomenon whose characterization has to be done not only on a yearly-basis but also on a seasonal and monthly basis. In the present paper, cloud attenuation statistics are reported at 20 GHz, 40 GHz and 75 GHz during rainy and non-rainy seasons in El Alto, Bolivia, at 4065 m of altitude, using 3 years of radiosoundings (2016-2019). Cloud detection models have been used for the calculations, including Salonen, Salonen08, Decker and CldMod models, and results obtained are compared to those given by the global model of the ITU-R Rec. P.840. The results lead to conclude that zenith cloud attenuation during rainy season can reach maximum values between 0.15 and 0.45 dB (20 GHz), 0.55 and 1.5 dB (40 GHz), and 1.3 and 3.9 dB (75 GHz) depending on the model to be used. In comparison, during non-rainy season these values vary between 0.08 and 0.33 dB (20 GHz), 0.26 and 1.1 dB (40 GHz), and 0.62 and 2.6 dB (75 GHz). On the other hand, statistics based on CldMod model and, in a less extent, Decker model are close to the ones obtained using the ITU-R global model. These observations could open the possibility of further studies assessing the reliability of meteorological parameters in digital maps at high altitude sites, because these data are used in global propagation models.
安第斯山脉中部雨季和非雨季基于无线电探测的Ka、Q和W波段的云衰减:玻利维亚埃尔阿尔托的研究
随着频率的增加,卫星通信系统中的云衰减成为一个相关问题,因此,在计算链路可用性时必须考虑到云衰减。这种大气损害是一种可变的大气现象,其特征不仅要按年确定,而且要按季节和按月确定。本文利用3年(2016-2019年)的无线电探测数据,报告了玻利维亚El Alto在4065 m海拔的雨季和非雨季,20 GHz、40 GHz和75 GHz的云衰减统计数据。计算中使用了云探测模式,包括Salonen、Salonen08、Decker和CldMod模式,并将计算结果与ITU-R Rec. P.840的全球模式进行了比较。结果表明,雨季天顶云衰减在0.15 ~ 0.45 dB (20 GHz)、0.55 ~ 1.5 dB (40 GHz)和1.3 ~ 3.9 dB (75 GHz)之间的最大值取决于所使用的模式。相比之下,在非雨季,这些值分别在0.08 ~ 0.33 dB (20 GHz)、0.26 ~ 1.1 dB (40 GHz)和0.62 ~ 2.6 dB (75 GHz)之间变化。另一方面,基于CldMod模型的统计量和基于Decker模型的统计量在较小程度上接近于使用ITU-R全球模型的统计量。这些观测可能开启进一步研究评估高海拔地区数字地图气象参数可靠性的可能性,因为这些数据用于全球传播模型。
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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