Cloud attenuation: Difference between revisions

From Glossary of Meteorology
imported>Perlwikibot
(Created page with " {{TermHeader}} {{TermSearch}} <div class="termentry"> <div class="term"> == cloud attenuation == </div> <div class="definition"><div class="short_definition">Usually, ...")
imported>Perlwikibot
No edit summary
 
Line 9: Line 9:
   </div>
   </div>


<div class="definition"><div class="short_definition">Usually, the [[attenuation]] of [[microwave radiation]] by [[clouds]].</div><br/> <div class="paragraph">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  <div class="display-formula"><blockquote>[[File:ams2001glos-Ce20.gif|link=|center|ams2001glos-Ce20]]</blockquote></div>  where ''M'' (g m<sup>&minus;3</sup>) is the liquid [[water content]], &#x003c1; (g cm<sup>&minus;3</sup>) the [[density]] of water, &#x003bb; the wavelength,  and <div class="inline-formula">[[File:ams2001glos-Cex03.gif|link=|ams2001glos-Cex03]]</div>, where ''m''<sup>2</sup> 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) &times;  10<sup>&minus;2</sup>''M'' for water clouds, and (2 to 20) &times; 10<sup>&minus;2</sup>''M'' for ice clouds.</div><br/> </div>
<div class="definition"><div class="short_definition">Usually, the [[attenuation]] of [[microwave radiation]] by [[clouds]].</div><br/> <div class="paragraph">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  <div class="display-formula"><blockquote>[[File:ams2001glos-Ce20.gif|link=|center|ams2001glos-Ce20]]</blockquote></div>  where ''M'' (g m<sup>-3</sup>) is the liquid [[water content]], &#x003c1; (g cm<sup>-3</sup>) the [[density]] of water, &#x003bb; the wavelength,  and <div class="inline-formula">[[File:ams2001glos-Cex03.gif|link=|ams2001glos-Cex03]]</div>, where ''m''<sup>2</sup> 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) &times;  10<sup>-2</sup>''M'' for water clouds, and (2 to 20) &times; 10<sup>-2</sup>''M'' for ice clouds.</div><br/> </div>
</div>
</div>



Latest revision as of 13:52, 20 February 2012



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
ams2001glos-Ce20
where M (g m-3) is the liquid water content, ρ (g cm-3) the density of water, λ the wavelength, and
ams2001glos-Cex03
, 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.


Copyright 2024 American Meteorological Society (AMS). For permission to reuse any portion of this work, please contact permissions@ametsoc.org. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act (17 U.S. Code § 107) or that satisfies the conditions specified in Section 108 of the U.S.Copyright Act (17 USC § 108) does not require AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, require written permission or a license from AMS. Additional details are provided in the AMS Copyright Policy statement.