Cloud attenuation
From Glossary of Meteorology
cloud attenuation[edit | edit source]
For the centimeter wavelength band, clouds produce Rayleigh scattering. The attenuation is due largely to scattering, rather than absorption, for both ice and water clouds. The cloud attenuation for one-way transmission is where M (g m−3) is the liquid water content, ρ (g cm−3) the density of water, λ the wavelength, and , where m2 is the complex dielectric constant. The attenuation depends only on M, and in the range of wavelengths from 1 to 10 cm is approximately (1 to 100) × 10−2M for water clouds, and (2 to 20) × 10−2M for ice clouds.