Long‐Term Propagation Measurements in Madrid in a Q‐Band Satellite‐to‐Earth Link

ABSTRACT The Q/V band (40/50 GHz) is gaining interest as satellite operators will need larger bandwidth to be able to provide their services, which are experiencing an increasingly high demand. An accurate characterization of the satellite‐to‐Earth propagation channel is of paramount importance to guarantee a high level of quality of service, by apportioning the right amount of resources to the users. For this reason, assessing the impact of the atmospheric effects in the band is critical. In Europe, the propagation payload of the Alphasat satellite has allowed the development of critical experiments in the Q‐band (39.4 GHz). One of these propagation campaigns was carried out in Madrid, Spain, from 2014 to 2026, resulting in more than 10 years of measurements gathered. The main results of Q‐band attenuation and rainfall rate from the processed 10 years of measurements of this ongoing experiment are presented in this paper. Moreover, rainfall rate, excess, total, and gas attenuation results, as well as the yearly variability of their statistical distributions, are quantified and compared to the predictions of the corresponding ITU‐R model. The results show that high values of attenuation are expected in time percentages relevant for the design of satellite links. For example, 20 dB of attenuation is exceeded for 0.04% of the time. Also, a large year‐to‐year variability can be expected for the temperate climate of Madrid.

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Publication Details

Journal
International Journal of Satellite Communications and Networking
Published
2026-09-18
DOI
https://doi.org/10.1002/sat.70088
Primary Topic
Precipitation Measurement and Analysis
Type
article
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article

Long‐Term Propagation Measurements in Madrid in a Q‐Band Satellite‐to‐Earth Link

José Manuel Riera, Pedro García-del-Pino, Gustavo A. Siles, Domingo Pimienta‐del‐Valle
International Journal of Satellite Communications and Networking
Precipitation Measurement and Analysis
article

Long‐Term Propagation Measurements in Madrid in a Q‐Band Satellite‐to‐Earth Link

José Manuel Riera, Pedro García-del-Pino, Gustavo A. Siles, Domingo Pimienta‐del‐Valle
article en

Abstract

ABSTRACT The Q/V band (40/50 GHz) is gaining interest as satellite operators will need larger bandwidth to be able to provide their services, which are experiencing an increasingly high demand. An accurate characterization of the satellite‐to‐Earth propagation channel is of paramount importance to guarantee a high level of quality of service, by apportioning the right amount of resources to the users. For this reason, assessing the impact of the atmospheric effects in the band is critical. In Europe, the propagation payload of the Alphasat satellite has allowed the development of critical experiments in the Q‐band (39.4 GHz). One of these propagation campaigns was carried out in Madrid, Spain, from 2014 to 2026, resulting in more than 10 years of measurements gathered. The main results of Q‐band attenuation and rainfall rate from the processed 10 years of measurements of this ongoing experiment are presented in this paper. Moreover, rainfall rate, excess, total, and gas attenuation results, as well as the yearly variability of their statistical distributions, are quantified and compared to the predictions of the corresponding ITU‐R model. The results show that high values of attenuation are expected in time percentages relevant for the design of satellite links. For example, 20 dB of attenuation is exceeded for 0.04% of the time. Also, a large year‐to‐year variability can be expected for the temperate climate of Madrid.

International Journal of Satellite Communications and Networking
Universidad Privada Boliviana (BO), Universidad Politécnica de Madrid (ES)
Climate action
Openalex Percentile: Top 15%
Precipitation Measurement and Analysis
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Long‐Term Propagation Measurements in Madrid in a Q‐Band Satellite‐to‐Earth Link — José Manuel Riera, Pedro García-del-Pino, et al. · International Journal of Satellite Communications and Networking (2026) | TGRS Research Map | TGRS