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Project IEEE 802.16 Broadband Wireless Access Working Group Title Power-Law Parameters of Rain Specific Attenuation

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TLDR
In this paper, the power-law form of rain specific attenuation is expressed as α R k ⋅, where k and α are the powerlaw parameters, and R is the rain rate in mm/h.
Abstract
A fundamental quantity in the calculation of rain attenuation statistics is the specific attenuation (attenuation per unit distance). The power-law form of rain specific attenuation is very convenient and is commonly used. It is expressed as α R k ⋅ , where k and α are the power-law parameters, and R is the rain rate in mm/h. Limited number of power-law parameters were available in the technical literature for certain raindrop size distributions. Some of these parameters had reservations for rain-rate ranges. New power-law parameters for four different (gamma, lognormal, Laws and Parsons, and Marshall and Palmer) raindrop size distributions are made. For a rain temperature of 0 C, k and α with polarization dependence are presented here for rain rates from 0 to 150 mm/h over the frequency range of 100 5 − GHz.

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Citations
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Proposed parameters of specific rain attenuation prediction for Free Space Optics link operating in tropical region

TL;DR: New parameters for specific rain attenuation prediction model that represents tropical weather condition are proposed, derived from data measured in Malaysia and using methods recommended by ITU-R.
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Attenuation and Differential Attenuation of 5-cm-Wavelength Radiation in Melting Hail

TL;DR: In this paper, specific attenuation and specific differential attenuation of 5-cm-wavelength radiation (C band) is compared with measurements at 10-cm wavelength (S band), which are much less affected by attenuation.
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Rain attenuation prediction and modeling for line-of-sight links on terrestrial paths in South Africa

TL;DR: In this paper, different rain attenuation prediction models proposed by different authors on terrestrial paths are studied and compared on a monthly basis, as well with the measured upper and lower attenuation bounds for a 6.73-km line-of-sight link operating at 19.5 GHz in Durban.
References
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Scattering of radiowaves by a melting layer of precipitation in backward and forward directions

TL;DR: In this paper, the authors derived the size distribution of the melting snow particles, the thickness of a melting layer, the density of a dry snow particle, and the average dielectric constant of melting snow particle.
Journal ArticleDOI

Backward and forward scattering by the melting layer composed of spheroidal hydrometeors at 5-100 GHz

TL;DR: In this article, the behavior of the differential reflectivity, specific attenuation, and specific phase shift due to a melting layer composed of oblate-spheroidal hydrometeors is analyzed.
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