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Space communications with variable elevation angle faded by rain: Radio links to the Sun–Earth first Lagrangian point L 1
Author(s) -
Matricciani Emilio
Publication year - 2015
Publication title -
international journal of satellite communications and networking
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.388
H-Index - 39
eISSN - 1542-0981
pISSN - 1542-0973
DOI - 10.1002/sat.1134
Subject(s) - computer science , elevation angle , point (geometry) , elevation (ballistics) , lagrangian point , lagrangian , variable (mathematics) , radio frequency , space (punctuation) , telecommunications , remote sensing , geodesy , astronomy , physics , geology , mathematics , geometry , azimuth , mathematical analysis , mathematical physics , operating system
Summary 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. Copyright © 2015 John Wiley & Sons, Ltd.