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Rain fade

Radio frequency absorption


Summary

Radio frequency absorption

Rain fade refers primarily to the absorption of a microwave radio frequency (RF) signal by atmospheric rain, snow, or ice, and losses which are especially prevalent at frequencies above 11 GHz. It also refers to the degradation of a signal caused by the electromagnetic interference of the leading edge of a storm front. Rain fade can be caused by precipitation at the uplink or downlink location. It does not need to be raining at a location for it to be affected by rain fade, as the signal may pass through precipitation many miles away, especially if the satellite dish has a low look angle. From 5% to 20% of rain fade or satellite signal attenuation may also be caused by rain, snow, or ice on the uplink or downlink antenna reflector, radome, or feed horn. Rain fade is not limited to satellite uplinks or downlinks, as it can also affect terrestrial point-to-point microwave links (those on the Earth's surface).

The rain attenuation on satellite communication can be predicted using rain attenuation prediction models which lead to a suitable selection of the Fade Mitigation Technique (FMT). The rain attenuation prediction models require rainfall rate data which, in turn, can be obtained from in either the prediction rainfall maps, which may reflect inaccurate rain performance prediction, or by actual measured rainfall data that gives more accurate prediction and hence the appropriate selection of FMT. Substantially, the earth altitude above the sea level is an essential factor affecting the rain attenuation performance. The satellite system designers and channel providers should account for the rain impairments at their channel setup.

Possible ways to overcome the effects of rain fade are site diversity, uplink power control, variable rate encoding, and receiving antennas larger than the requested size for normal weather conditions.

CCIR interpolation formula

It is possible to extrapolate the cumulative attenuation distribution at a given location by using the CCIR interpolation formula:CCIR [1990] Report 564-4 "Propagation data and prediction methods required for earth-space telecommunication systems"

: A**p = A001 0.12 p−(0.546 − 0.0043 log10 p).

where A**p is the attenuation in dB exceeded for a p percentage of the time and A001 is the attenuation exceeded for 0.01% of the time.

ITU-R frequency scaling formula

According to the ITU-R, rain attenuation statistics can be scaled in frequency in the range 7 to 55 GHz by the formula

:\frac{A_2}{A_1} = \left(\frac{b_2}{b_1}\right) ^ {1-1.12 \cdot 10^{-3}\sqrt{b_2/b_1}(b_1A_1)^{0.55}}

where

:b_i = \frac{f_i^2}{1+10^{-4} f_i^2}

and f is the frequency in GHz.

References

References

  1. (2021). "Rainfall Effect on Satellite Communications in Mosul at Frequencies above 10 GHz".
  2. (2020-05-01). "Direct extraction of rain-induced impairments on satellite communication channel in subtropical climate at K and Ka bands". Telecommunication Systems.
  3. (May 1, 2021). "Rain Fade".
  4. (January 2021). "A Survey of Rain Fade Models for Earth–Space Telecommunication Links—Taxonomy, Methods, and Comparative Study". Remote Sensing.
  5. "Uplink power control method and apparatus for satellite communications networks".
  6. "Diversity in Microwave Links".
  7. (2015-04-13). "Microwave Link".
  8. (2017-11-28). "Point to Point Archives - Page 2 of 3".
  9. “Propagation Data and Prediction Methods Required for the Design of Earth-Space Telecommunication Systems,” Recommendations of the ITU-R, Rec. P.618-10, 2009.
Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

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