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Space communications with variable elevation angle faded by rain: Radio links to the Sun-Earth first Lagrangian point L_1

机译:倾角因雨而减弱的空间通信:到日地第一拉格朗日点L_1的无线电链路

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How rain attenuation affects space links with variable elevation angles is not yet fully researched. The aim of this paper is to investigate this topic by simulating rain attenuation at K_a Band, in slant paths with variable elevation angles, with the Synthetic Storm Technique (SST), in links connected with spacecrafts at the Sun-Earth first Lagrangian point L_1 viewed from Spino d'Adda (Italy), Tampa (Florida), White Sands (New Mexico). The input to the SST is a large database of time series of 1-min rain rate recorded on site, 10 years in Spino d'Adda, 4 years at Tampa and White Sands. After recalling known results on the elevation angle of the Sun (i.e. L_1),θ_s(°), seen from latitude λ (°), I report what seems to be a new result: the mode of the probability density function of θ_s in a year, in the range 0 ≤ λ ≤ 90° - ε (Earth axis tilt angle ε=23.44°), coincides with the peak angle found at the day of the Winter solstice at the site, a result valid also for other planets, once their tilt angle is used. Compared to the complementary probability distribution function (pdf) of rain attenuation calculated for a geostationary (GEO) link (fixed elevation angle), the pdf to L_1 depends on the rain-rate pdf during the contact time with L_1; according to the local climate. I show that, to obtain a good and easier estimate of the rain attenuation pdf in L_1 links, we can consider a GEO link with elevation angle equal to the mean angle and rain rate pdf, both during the contact time, and that the mode angle gives an upper bound to the rain attenuation pdf in the sites considered.
机译:降雨衰减如何影响具有可变仰角的空间链接的方式尚未完全研究。本文的目的是通过利用合成风暴技术(SST)在太阳地球第一个拉格朗日点L_1上与航天器连接的链路中模拟K_a波段,具有不同仰角的倾斜路径中的降雨衰减来研究此主题来自Spino d'Adda(意大利),坦帕(佛罗里达),白沙(新墨西哥)。 SST的输入是一个大型的数据库,该数据库在现场记录了1分钟降雨率的时间序列,在Spino d'Adda为10年,在Tampa和White Sands为4年。回顾了从仰角λ(°)观察到的关于太阳仰角(即L_1),θ_s(°)的已知结果之后,我报告了似乎是一个新的结果:θ_s的概率密度函数的模式年份,在0≤λ≤90°-ε(地轴倾斜角ε= 23.44°)的范围内,与该冬至当天在该地点发现的峰值角一致,这一结果对其他行星也一次有效使用它们的倾斜角度。与为对地静止(GEO)链路(固定仰角)计算的降雨衰减的互补概率分布函数(pdf)相比,L_1的pdf取决于与L_1接触期间的降雨率pdf;根据当地气候。我表明,为了获得更好且更容易的L_1链接中降雨衰减pdf的估计值,我们可以考虑在接触时间和模式角度下仰角等于平均角度和降雨率pdf的GEO链接给出了所考虑地点的降雨衰减pdf的上限。

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